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	<id>https://wiki.signal-earth.org/index.php?action=history&amp;feed=atom&amp;title=Sea_surface_temperature_%28global_mean%29</id>
	<title>Sea surface temperature (global mean) - Revision history</title>
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	<updated>2026-06-01T13:25:30Z</updated>
	<subtitle>Revision history for this page on the wiki</subtitle>
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		<id>https://wiki.signal-earth.org/index.php?title=Sea_surface_temperature_(global_mean)&amp;diff=35&amp;oldid=prev</id>
		<title>Rtuffli: SIGNAL publish from draft v12</title>
		<link rel="alternate" type="text/html" href="https://wiki.signal-earth.org/index.php?title=Sea_surface_temperature_(global_mean)&amp;diff=35&amp;oldid=prev"/>
		<updated>2026-05-29T18:30:27Z</updated>

		<summary type="html">&lt;p&gt;SIGNAL publish from draft v12&lt;/p&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 18:30, 29 May 2026&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l23&quot;&gt;Line 23:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 23:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;!-- SIGNAL_EARTH_INFOBOX_END --&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;!-- SIGNAL_EARTH_INFOBOX_END --&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;{{SignalTerm|type=DS|id=DS-00002|label=Sea surface temperature (global mean)}} Sea surface temperature (SST) represents the temperature of the ocean&#039;s surface layer and is a fundamental parameter in &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the study of &lt;/del&gt;Earth&#039;s climate system. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Variations in SST influence &lt;/del&gt;atmospheric circulation, weather patterns, and marine ecosystems &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;globally&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Monitoring global mean &lt;/del&gt;SST &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;provides insights into oceanic heat content, climate variability, and long&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;term trends associated with natural &lt;/del&gt;and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;anthropogenic factors&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;{{SignalTerm|type=DS|id=DS-00002|label=Sea surface temperature (global mean)}} &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[https://en.wikipedia.org/wiki/Sea_surface_temperature &lt;/ins&gt;Sea surface temperature&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;] &lt;/ins&gt;(SST) represents the temperature of the ocean&#039;s surface layer and is a fundamental parameter in &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;understanding &lt;/ins&gt;Earth&#039;s climate system. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;The global mean sea surface temperature reflects the average thermal state of the ocean surface worldwide, influencing &lt;/ins&gt;atmospheric circulation, weather patterns, and marine ecosystems. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Variations in &lt;/ins&gt;SST &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;are closely linked to phenomena such as El Niño&lt;/ins&gt;-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Southern Oscillation &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;play a critical role in the global energy balance&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;The &lt;/del&gt;global mean &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;sea surface temperature integrates measurements from the world&#039;s oceans&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;offering a comprehensive indicator of oceanic thermal state. This parameter is critical for understanding phenomena such as El Niño-Southern Oscillation, tropical cyclone development&lt;/del&gt;, and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ocean&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;atmosphere heat exchange processes&lt;/del&gt;. It &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;also serves as an essential input for &lt;/del&gt;climate &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;models &lt;/del&gt;and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;environmental assessments&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Monitoring &lt;/ins&gt;global mean &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;SST provides insights into ocean heat content changes&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;climate variability&lt;/ins&gt;, and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;long&lt;/ins&gt;-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;term trends associated with climate change&lt;/ins&gt;. It &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;is a key indicator used in &lt;/ins&gt;climate &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;assessments and oceanographic research. The measurement of SST integrates data from multiple platforms to capture spatial &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;temporal variability across the world&#039;s oceans&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Within the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;broader &lt;/del&gt;context of &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ocean-physical studies&lt;/del&gt;, global mean SST &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;acts &lt;/del&gt;as a state variable &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;reflecting the current condition of &lt;/del&gt;the ocean &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;surface environment. Its continuous observation supports scientific research&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;environmental monitoring, and the evaluation of climate change impacts &lt;/del&gt;on &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;marine &lt;/del&gt;and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;atmospheric &lt;/del&gt;systems.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Within the context of &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;environmental monitoring&lt;/ins&gt;, global mean SST &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;serves &lt;/ins&gt;as a state variable &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;within &lt;/ins&gt;the ocean&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;-physical domain&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;reflecting changes in oceanic conditions that can have cascading effects &lt;/ins&gt;on &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;atmospheric &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ecological &lt;/ins&gt;systems.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Geographic / System Context ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Geographic / System Context ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The global mean sea surface temperature encompasses the entire surface &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;layer &lt;/del&gt;of &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the world&#039;s oceans&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;including &lt;/del&gt;major basins &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;such as &lt;/del&gt;the Pacific, Atlantic, Indian, Southern, and Arctic Oceans. This &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;broad &lt;/del&gt;geographic scope captures &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;spatial variability across tropical&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;temperate&lt;/del&gt;, and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;polar regions&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Ocean &lt;/del&gt;surface &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;waters interact dynamically with &lt;/del&gt;the atmosphere&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, sea ice&lt;/del&gt;, and coastal zones, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;influencing regional climates &lt;/del&gt;and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;biogeochemical cycles&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;The &lt;/del&gt;global &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;aggregation integrates these &lt;/del&gt;diverse &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;oceanic &lt;/del&gt;environments &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;to provide a unified metric of surface thermal conditions&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The global mean sea surface temperature encompasses the entire &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;oceanic &lt;/ins&gt;surface of &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Earth&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;spanning all &lt;/ins&gt;major &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ocean &lt;/ins&gt;basins &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;including &lt;/ins&gt;the Pacific, Atlantic, Indian, Southern, and Arctic Oceans. This &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;extensive &lt;/ins&gt;geographic scope captures &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;temperature variations influenced by latitude&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ocean currents, seasonal cycles&lt;/ins&gt;, and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;regional climatic events&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;The ocean &lt;/ins&gt;surface &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;acts as a dynamic interface between &lt;/ins&gt;the atmosphere &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and the ocean interior&lt;/ins&gt;, and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;SST patterns vary with geographic features such as &lt;/ins&gt;coastal zones, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;upwelling regions, &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;equatorial waters&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Understanding SST at a &lt;/ins&gt;global &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;scale requires integrating data across &lt;/ins&gt;diverse &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;marine &lt;/ins&gt;environments &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and climatic zones&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Monitoring and Measurement ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Monitoring and Measurement ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Sea surface temperature is &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;monitored &lt;/del&gt;using a combination of satellite remote sensing, in situ measurements from buoys, ships, and floats, and blended &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;analysis products. Key monitoring institutions include the Copernicus Marine Environment Monitoring Service and the National Oceanic and Atmospheric Administration (NOAA)&lt;/del&gt;. Satellite &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;sensors measure &lt;/del&gt;thermal infrared and microwave emissions from the ocean surface&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, providing high spatial and temporal resolution data&lt;/del&gt;. In situ observations calibrate and validate satellite &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;retrievals, ensuring accuracy and continuity&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Established datasets &lt;/del&gt;such as the NOAA Optimum Interpolation Sea Surface Temperature (OISST) and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the &lt;/del&gt;Extended Reconstructed Sea Surface Temperature (ERSST) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;provide long-term&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;quality&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;controlled &lt;/del&gt;SST &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;records essential &lt;/del&gt;for climate research.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Sea surface temperature is &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;observed &lt;/ins&gt;using a combination of satellite remote sensing, in situ measurements from buoys, ships, and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;autonomous &lt;/ins&gt;floats, and blended &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;analyses that integrate multiple data sources&lt;/ins&gt;. Satellite &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;instruments provide broad spatial coverage with frequent revisits, measuring &lt;/ins&gt;thermal infrared and microwave emissions from the ocean surface. In situ observations &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;offer direct temperature measurements that &lt;/ins&gt;calibrate and validate satellite &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;data&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Monitoring institutions &lt;/ins&gt;such as the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;National Oceanic and Atmospheric Administration ([https://en.wikipedia.org/wiki/National_Oceanic_and_Atmospheric_Administration &lt;/ins&gt;NOAA&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]) and the European Copernicus program maintain operational SST products, including the &lt;/ins&gt;Optimum Interpolation Sea Surface Temperature (OISST) and Extended Reconstructed Sea Surface Temperature (ERSST) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;datasets. These products apply statistical methods to merge observations and generate continuous&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;high&lt;/ins&gt;-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;resolution &lt;/ins&gt;SST &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;fields suitable &lt;/ins&gt;for climate &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;monitoring and &lt;/ins&gt;research.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Within the SIGNAL system, this phenomenon is treated as a defined environmental signal whose boundaries and measurement conventions are described below.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Within the SIGNAL system, this phenomenon is treated as a defined environmental signal whose boundaries and measurement conventions are described below.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Signal Definition ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Signal Definition ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;sea &lt;/del&gt;surface temperature (global mean) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;signal &lt;/del&gt;is &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;defined as &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;spatially averaged &lt;/del&gt;temperature of the ocean&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&#039;s &lt;/del&gt;surface layer, expressed in degrees Celsius (°C)&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;. It represents a continuous temporal state variable within the Ocean-Physical domain, derived from the observable type &#039;Sea surface temperature&#039;&lt;/del&gt;. This signal captures the thermal &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;condition &lt;/del&gt;of the ocean surface &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;at &lt;/del&gt;a &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;global scale &lt;/del&gt;and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;serves as an indicator of oceanic heat content and climate variability&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Sea &lt;/ins&gt;surface temperature (global mean) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Damage Signal &lt;/ins&gt;is &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;derived from the Observable Type &#039;Sea surface temperature&#039; and represents a continuous state condition within the Ocean-Physical domain. It quantifies &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;average &lt;/ins&gt;temperature of the ocean surface layer &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;globally&lt;/ins&gt;, expressed in degrees Celsius (°C). This signal captures the thermal &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;state &lt;/ins&gt;of the ocean surface &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;as &lt;/ins&gt;a &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;physical stressor influencing climate &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;environmental processes&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Boundary Conditions ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Boundary Conditions ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Boundary inclusions encompass all ocean surface waters globally, integrating temperature measurements from &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;open &lt;/del&gt;ocean&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, coastal zones, and marginal seas&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;The signal excludes non-oceanic &lt;/del&gt;water bodies &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;such as inland lakes and rivers. Sea &lt;/del&gt;ice-covered &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;regions are generally excluded from &lt;/del&gt;direct SST measurement &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;due to ice presence&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;though adjacent open waters are included. Vertical boundaries are limited to &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ocean&#039;s &lt;/del&gt;surface layer&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, typically &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;upper few millimeters to meters, where &lt;/del&gt;temperature &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;exchanges with &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;atmosphere occur. Temporal boundaries are continuous&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;capturing daily to decadal variations without interruption&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Boundary inclusions &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;for this signal &lt;/ins&gt;encompass all ocean surface waters globally, integrating temperature measurements from &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the uppermost &lt;/ins&gt;ocean &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;layer typically within the top few millimeters to meters where thermal exchange with the atmosphere occurs&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Boundary exclusions include inland &lt;/ins&gt;water bodies&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, sea &lt;/ins&gt;ice-covered &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;surfaces where &lt;/ins&gt;direct SST measurement &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;is not applicable&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and subsurface ocean temperatures below &lt;/ins&gt;the surface layer&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;. Coastal land areas and terrestrial temperature measurements are excluded. The signal focuses solely on &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;physical &lt;/ins&gt;temperature &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;state of &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ocean surface&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;excluding chemical or biological parameters&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Aggregation Semantics ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Aggregation Semantics ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Geographically, &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;signal aggregates sea &lt;/del&gt;surface &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;temperature measurements across &lt;/del&gt;all &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;oceanic &lt;/del&gt;regions &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;worldwide to produce a global mean value&lt;/del&gt;. Temporal aggregation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;involves &lt;/del&gt;continuous &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;monitoring &lt;/del&gt;with &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;data &lt;/del&gt;often &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;averaged over &lt;/del&gt;daily, monthly, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;or &lt;/del&gt;annual &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;intervals &lt;/del&gt;to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;identify &lt;/del&gt;trends &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and variability&lt;/del&gt;. Cross-signal aggregation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;considers correlations &lt;/del&gt;with related environmental signals such as atmospheric greenhouse gas concentrations &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and cryospheric changes &lt;/del&gt;to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;understand &lt;/del&gt;coupled &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;system &lt;/del&gt;dynamics. Aggregation methods &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;apply statistical weighting to account for &lt;/del&gt;spatial &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;sampling density &lt;/del&gt;and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;measurement uncertainties, ensuring representative global estimates&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Geographic aggregation for this signal involves spatial averaging over &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;global ocean &lt;/ins&gt;surface&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, encompassing &lt;/ins&gt;all &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ocean basins and &lt;/ins&gt;regions. Temporal aggregation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;is &lt;/ins&gt;continuous&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, &lt;/ins&gt;with &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;datasets &lt;/ins&gt;often &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;providing &lt;/ins&gt;daily, monthly, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and &lt;/ins&gt;annual &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;averages &lt;/ins&gt;to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;capture both short-term variability and long-term &lt;/ins&gt;trends. Cross-signal aggregation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;may involve integrating SST data &lt;/ins&gt;with related environmental signals such as atmospheric greenhouse gas concentrations &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;or ocean oxygen levels &lt;/ins&gt;to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;assess &lt;/ins&gt;coupled &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;climate and ecosystem &lt;/ins&gt;dynamics. Aggregation methods &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ensure consistent representation of the global ocean surface temperature state while accommodating &lt;/ins&gt;spatial &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;heterogeneity &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;temporal fluctuations&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Observational Status ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Observational Status ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Global mean sea surface temperature is actively monitored &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;with &lt;/del&gt;well-established observational networks and data products &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;maintained by agencies &lt;/del&gt;such as NOAA and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the Copernicus program. Long-term datasets enable assessment of historical trends &lt;/del&gt;and climate &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;variability. Ongoing improvements in satellite sensor technology and data assimilation techniques enhance spatial &lt;/del&gt;and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;temporal resolution&lt;/del&gt;. Future SIGNAL releases may incorporate &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;higher-&lt;/del&gt;resolution &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;regional analyses&lt;/del&gt;, integration with &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;additional environmental signals, &lt;/del&gt;and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;refined uncertainty quantification &lt;/del&gt;to support comprehensive &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ocean-climate &lt;/del&gt;assessments.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Global mean sea surface temperature is actively monitored &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;through &lt;/ins&gt;well-established observational networks and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;satellite missions, producing continuous datasets that span multiple decades. Current &lt;/ins&gt;data products&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, &lt;/ins&gt;such as NOAA&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&#039;s OISST &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ERSST, provide validated &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;widely used SST records for &lt;/ins&gt;climate &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;research &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;operational applications&lt;/ins&gt;. Future SIGNAL releases may incorporate &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;enhanced spatial &lt;/ins&gt;resolution, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;improved data assimilation techniques, and &lt;/ins&gt;integration with &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;emerging observational platforms to refine the characterization of SST variability and trends. Ongoing efforts aim to reduce uncertainties &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;extend historical reconstructions &lt;/ins&gt;to support comprehensive &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;environmental &lt;/ins&gt;assessments.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Related Signals ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Related Signals ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l69&quot;&gt;Line 69:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 69:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;!-- SIGNAL_EARTH_SOURCES_START --&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;!-- SIGNAL_EARTH_SOURCES_START --&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Sources ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Sources ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;{{cite web | title=NOAA NCEI Optimum Interpolation Sea Surface Temperature (OISST) product page | url=&lt;/del&gt;https://www.ncei.noaa.gov/products/optimum-interpolation-sst &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;| publisher=&lt;/del&gt;NOAA NCEI &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;| year=&lt;/del&gt;2026&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;}}&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[&lt;/ins&gt;https://www.ncei.noaa.gov/products/optimum-interpolation-sst NOAA NCEI &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Optimum Interpolation Sea Surface Temperature (OISST) product page — &lt;/ins&gt;2026 &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;— NOAA NCEI]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;{{cite journal | title=&lt;/del&gt;Extended Reconstructed Sea Surface Temperature, Version 5 (ERSSTv5): Upgrades, Validations, and Intercomparisons &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;| journal=&lt;/del&gt;Journal of Climate &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;| year=2017 | doi=10.1175/JCLI-D-16-0836.1 | url=&lt;/del&gt;https://doi.org/10.1175/&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;JCLI-D-16-0836&lt;/del&gt;.1&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;}}&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[https://doi.org/10.1175/JCLI-D-16-0836.1 &lt;/ins&gt;Extended Reconstructed Sea Surface Temperature, Version 5 (ERSSTv5): Upgrades, Validations, and Intercomparisons &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;— 2017 — &lt;/ins&gt;Journal of Climate&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* {{cite journal | title=&lt;/del&gt;Daily High-Resolution-Blended Analyses for Sea Surface Temperature &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;| journal=&lt;/del&gt;Journal of Climate &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;| year=2007 | doi=10.1175/2007JCLI1824.1 | url=&lt;/del&gt;https://doi.org/10.&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;1175&lt;/del&gt;/&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;2007JCLI1824.1}}&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* [&lt;/ins&gt;https://doi.org/10.1175/&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;2007JCLI1824&lt;/ins&gt;.1 Daily High-Resolution-Blended Analyses for Sea Surface Temperature &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;— 2007 — &lt;/ins&gt;Journal of Climate&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* {{cite journal | title=&lt;/del&gt;Global analyses of sea surface temperature, sea-ice and night marine air temperature since the late nineteenth century &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;| journal=&lt;/del&gt;JGR Atmospheres &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;| year=2003 | doi=10.1029/2002JD002670 | url=https://doi.org/10.1029/2002JD002670}}&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;* [&lt;/ins&gt;https://doi.org/10.&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;1029&lt;/ins&gt;/&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;2002JD002670 &lt;/ins&gt;Global analyses of sea surface temperature, sea-ice and night marine air temperature since the late nineteenth century &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;— 2003 — &lt;/ins&gt;JGR Atmospheres&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;!-- SIGNAL_EARTH_SOURCES_END --&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;!-- SIGNAL_EARTH_SOURCES_END --&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Rtuffli</name></author>
	</entry>
	<entry>
		<id>https://wiki.signal-earth.org/index.php?title=Sea_surface_temperature_(global_mean)&amp;diff=34&amp;oldid=prev</id>
		<title>Rtuffli: SIGNAL publish from draft v10</title>
		<link rel="alternate" type="text/html" href="https://wiki.signal-earth.org/index.php?title=Sea_surface_temperature_(global_mean)&amp;diff=34&amp;oldid=prev"/>
		<updated>2026-05-29T17:47:18Z</updated>

		<summary type="html">&lt;p&gt;SIGNAL publish from draft v10&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 17:47, 29 May 2026&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l23&quot;&gt;Line 23:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 23:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;!-- SIGNAL_EARTH_INFOBOX_END --&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;!-- SIGNAL_EARTH_INFOBOX_END --&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;{{SignalTerm|type=DS|id=DS-00002|label=Sea surface temperature (global mean)}} Sea surface temperature (SST) represents the temperature of the ocean&#039;s surface layer and is a fundamental parameter in the study of climate &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and oceanographic processes&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;It influences &lt;/del&gt;atmospheric circulation, weather patterns, and marine ecosystems. Monitoring global mean SST provides &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;critical &lt;/del&gt;insights into &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ocean &lt;/del&gt;heat content and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the Earth&#039;s energy balance&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;{{SignalTerm|type=DS|id=DS-00002|label=Sea surface temperature (global mean)}} Sea surface temperature (SST) represents the temperature of the ocean&#039;s surface layer and is a fundamental parameter in the study of &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Earth&#039;s &lt;/ins&gt;climate &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;system&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Variations in SST influence &lt;/ins&gt;atmospheric circulation, weather patterns, and marine ecosystems &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;globally&lt;/ins&gt;. Monitoring global mean SST provides insights into &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;oceanic &lt;/ins&gt;heat content&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, climate variability, and long-term trends associated with natural &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;anthropogenic factors&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Variations in &lt;/del&gt;sea surface temperature &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;are linked to &lt;/del&gt;phenomena such as El Niño &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and La Niña&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;which have widespread climatic impacts. SST changes can affect marine biodiversity, fisheries&lt;/del&gt;, and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;coral reef health&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Understanding SST trends is &lt;/del&gt;essential for &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;assessing the responses of the ocean-atmosphere system to natural variability &lt;/del&gt;and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;anthropogenic influences&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;The global mean &lt;/ins&gt;sea surface temperature &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;integrates measurements from the world&#039;s oceans, offering a comprehensive indicator of oceanic thermal state. This parameter is critical for understanding &lt;/ins&gt;phenomena such as El Niño&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;-Southern Oscillation&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;tropical cyclone development&lt;/ins&gt;, and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ocean-atmosphere heat exchange processes&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;It also serves as an &lt;/ins&gt;essential &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;input &lt;/ins&gt;for &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;climate models &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;environmental assessments&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;This article describes &lt;/del&gt;the global mean &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;sea surface temperature &lt;/del&gt;as &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;an environmental signal within &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;SIGNAL Earth observatory system&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;outlining its measurement, definition&lt;/del&gt;, and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;contextual relevance&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Within &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;broader context of ocean-physical studies, &lt;/ins&gt;global mean &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;SST acts &lt;/ins&gt;as &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;a state variable reflecting the current condition of &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ocean surface environment. Its continuous observation supports scientific research&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;environmental monitoring&lt;/ins&gt;, and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the evaluation of climate change impacts on marine and atmospheric systems&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Geographic / System Context ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Geographic / System Context ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Sea &lt;/del&gt;surface temperature &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;is measured across &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;global ocean&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;encompassing all &lt;/del&gt;major &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ocean &lt;/del&gt;basins &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;including &lt;/del&gt;the Atlantic&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, Pacific&lt;/del&gt;, Indian, Southern, and Arctic Oceans. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;The ocean &lt;/del&gt;surface &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;layer interacts &lt;/del&gt;with the atmosphere &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and is influenced by regional and global circulation patterns&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar radiation&lt;/del&gt;, and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;heat exchange processes. Variability in SST occurs at multiple spatial scales, from local &lt;/del&gt;coastal zones &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;to basin-wide &lt;/del&gt;and global &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;scales, reflecting both natural climate variability and long-term trends&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;The global mean sea &lt;/ins&gt;surface temperature &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;encompasses the entire surface layer of &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;world&#039;s oceans&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;including &lt;/ins&gt;major basins &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;such as &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Pacific, &lt;/ins&gt;Atlantic, Indian, Southern, and Arctic Oceans. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;This broad geographic scope captures spatial variability across tropical, temperate, and polar regions. Ocean &lt;/ins&gt;surface &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;waters interact dynamically &lt;/ins&gt;with the atmosphere, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;sea ice&lt;/ins&gt;, and coastal zones&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, influencing regional climates &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;biogeochemical cycles. The &lt;/ins&gt;global &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;aggregation integrates these diverse oceanic environments to provide a unified metric of surface thermal conditions&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Monitoring and Measurement ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Monitoring and Measurement ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Sea surface temperature is monitored &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;through &lt;/del&gt;a combination of satellite remote sensing, in situ measurements from buoys, ships, and floats, and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;reanalysis &lt;/del&gt;products. Key monitoring institutions include the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[&lt;/del&gt;National Oceanic and Atmospheric Administration&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;|&lt;/del&gt;NOAA&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]] &lt;/del&gt;and the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;European Union&#039;s [[Copernicus Programme|Copernicus]] service. Satellite instruments provide &lt;/del&gt;high&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;-&lt;/del&gt;resolution, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;near-global coverage of SST, while in situ data offer calibration &lt;/del&gt;and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;validation&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Products &lt;/del&gt;such as the Optimum Interpolation Sea Surface Temperature (OISST) and the Extended Reconstructed Sea Surface Temperature (ERSST) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;datasets integrate these observations to produce consistent time series &lt;/del&gt;for climate &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;analysis&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Sea surface temperature is monitored &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;using &lt;/ins&gt;a combination of satellite remote sensing, in situ measurements from buoys, ships, and floats, and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;blended analysis &lt;/ins&gt;products. Key monitoring institutions include the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Copernicus Marine Environment Monitoring Service and the &lt;/ins&gt;National Oceanic and Atmospheric Administration &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;(&lt;/ins&gt;NOAA&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;). Satellite sensors measure thermal infrared &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;microwave emissions from &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ocean surface, providing &lt;/ins&gt;high &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;spatial and temporal &lt;/ins&gt;resolution &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;data. In situ observations calibrate and validate satellite retrievals&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ensuring accuracy &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;continuity&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Established datasets &lt;/ins&gt;such as the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;NOAA &lt;/ins&gt;Optimum Interpolation Sea Surface Temperature (OISST) and the Extended Reconstructed Sea Surface Temperature (ERSST) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;provide long-term, quality-controlled SST records essential &lt;/ins&gt;for climate &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;research&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Within the SIGNAL system, this phenomenon is treated as a defined environmental signal whose boundaries and measurement conventions are described below.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Within the SIGNAL system, this phenomenon is treated as a defined environmental signal whose boundaries and measurement conventions are described below.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Signal Definition ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Signal Definition ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The sea surface temperature (global mean) signal &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;represents &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;average &lt;/del&gt;temperature of the ocean&#039;s surface layer, expressed in degrees Celsius (°C). It &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;is &lt;/del&gt;derived from the observable type &#039;Sea surface temperature&#039; &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and quantifies the state of the ocean&#039;s uppermost thermal environment on a global scale&lt;/del&gt;. This signal &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;reflects &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;integrated &lt;/del&gt;thermal condition of the ocean surface &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;over time &lt;/del&gt;and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;space&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The sea surface temperature (global mean) signal &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;is defined as &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;spatially averaged &lt;/ins&gt;temperature of the ocean&#039;s surface layer, expressed in degrees Celsius (°C). It &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;represents a continuous temporal state variable within the Ocean-Physical domain, &lt;/ins&gt;derived from the observable type &#039;Sea surface temperature&#039;. This signal &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;captures &lt;/ins&gt;the thermal condition of the ocean surface &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;at a global scale and serves as an indicator of oceanic heat content &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;climate variability&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Boundary Conditions ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Boundary Conditions ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Boundary inclusions encompass &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the &lt;/del&gt;temperature measurements &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;of &lt;/del&gt;the ocean surface layer, typically the upper few millimeters to meters &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;of the ocean&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;averaged across all global oceanic regions. Boundary exclusions include temperatures from subsurface layers below &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;surface skin layer, inland water bodies such as lakes and rivers, and coastal land areas&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;The signal excludes atmospheric temperature measurements and sea ice surface temperatures&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;focusing solely on liquid ocean surface waters&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Boundary inclusions encompass &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;all ocean surface waters globally, integrating &lt;/ins&gt;temperature measurements &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;from open ocean, coastal zones, and marginal seas. The signal excludes non-oceanic water bodies such as inland lakes and rivers. Sea ice-covered regions are generally excluded from direct SST measurement due to ice presence, though adjacent open waters are included. Vertical boundaries are limited to &lt;/ins&gt;the ocean&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&#039;s &lt;/ins&gt;surface layer, typically the upper few millimeters to meters, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;where temperature exchanges with &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;atmosphere occur&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Temporal boundaries are continuous&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;capturing daily to decadal variations without interruption&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Aggregation Semantics ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Aggregation Semantics ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Geographic aggregation involves averaging &lt;/del&gt;sea surface temperature &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;data &lt;/del&gt;across &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the entire &lt;/del&gt;global &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ocean surface, integrating measurements from all ocean basins&lt;/del&gt;. Temporal aggregation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;is &lt;/del&gt;continuous&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, &lt;/del&gt;with data &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;compiled and &lt;/del&gt;averaged over daily, monthly, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;seasonal, and &lt;/del&gt;annual intervals to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;capture both short-term &lt;/del&gt;variability &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and long-term trends&lt;/del&gt;. Cross-signal aggregation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;may involve correlating global mean SST &lt;/del&gt;with related environmental signals such as atmospheric greenhouse gas concentrations and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;cryosphere indicators &lt;/del&gt;to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;assess &lt;/del&gt;coupled &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;climate &lt;/del&gt;system dynamics.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Geographically, the signal aggregates &lt;/ins&gt;sea surface temperature &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;measurements &lt;/ins&gt;across &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;all oceanic regions worldwide to produce a &lt;/ins&gt;global &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;mean value&lt;/ins&gt;. Temporal aggregation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;involves &lt;/ins&gt;continuous &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;monitoring &lt;/ins&gt;with data &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;often &lt;/ins&gt;averaged over daily, monthly, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;or &lt;/ins&gt;annual intervals to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;identify trends and &lt;/ins&gt;variability. Cross-signal aggregation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;considers correlations &lt;/ins&gt;with related environmental signals such as atmospheric greenhouse gas concentrations and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;cryospheric changes &lt;/ins&gt;to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;understand &lt;/ins&gt;coupled system dynamics&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;. Aggregation methods apply statistical weighting to account for spatial sampling density and measurement uncertainties, ensuring representative global estimates&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Observational Status ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Observational Status ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Global mean sea surface temperature is &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;continuously &lt;/del&gt;monitored with &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;extensive historical &lt;/del&gt;and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;contemporary datasets available. Current &lt;/del&gt;products such as NOAA&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&#039;s OISST provide high&lt;/del&gt;-&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;resolution, blended analyses that integrate &lt;/del&gt;satellite and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;in situ &lt;/del&gt;data. Future SIGNAL releases may &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;enhance temporal and spatial &lt;/del&gt;resolution, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;incorporate emerging observational platforms&lt;/del&gt;, and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;refine &lt;/del&gt;uncertainty quantification&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;. Ongoing validation and intercomparison efforts &lt;/del&gt;support &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the reliability of SST data within the SIGNAL framework&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Global mean sea surface temperature is &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;actively &lt;/ins&gt;monitored with &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;well-established observational networks &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;data &lt;/ins&gt;products &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;maintained by agencies &lt;/ins&gt;such as NOAA &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and the Copernicus program. Long&lt;/ins&gt;-&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;term datasets enable assessment of historical trends and climate variability. Ongoing improvements in &lt;/ins&gt;satellite &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;sensor technology &lt;/ins&gt;and data &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;assimilation techniques enhance spatial and temporal resolution&lt;/ins&gt;. Future SIGNAL releases may &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;incorporate higher-&lt;/ins&gt;resolution &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;regional analyses&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;integration with additional environmental signals&lt;/ins&gt;, and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;refined &lt;/ins&gt;uncertainty quantification &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;to &lt;/ins&gt;support &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;comprehensive ocean-climate assessments&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Related Signals ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Related Signals ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Rtuffli</name></author>
	</entry>
	<entry>
		<id>https://wiki.signal-earth.org/index.php?title=Sea_surface_temperature_(global_mean)&amp;diff=33&amp;oldid=prev</id>
		<title>Rtuffli: SIGNAL publish from draft v8</title>
		<link rel="alternate" type="text/html" href="https://wiki.signal-earth.org/index.php?title=Sea_surface_temperature_(global_mean)&amp;diff=33&amp;oldid=prev"/>
		<updated>2026-05-29T17:27:36Z</updated>

		<summary type="html">&lt;p&gt;SIGNAL publish from draft v8&lt;/p&gt;
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				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 17:27, 29 May 2026&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l23&quot;&gt;Line 23:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 23:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;!-- SIGNAL_EARTH_INFOBOX_END --&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;!-- SIGNAL_EARTH_INFOBOX_END --&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;{{SignalTerm|type=DS|id=DS-00002|label=Sea surface temperature (global mean)}} Sea surface temperature (SST) represents the temperature of the ocean&#039;s surface layer and is a &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;critical &lt;/del&gt;parameter in &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;understanding Earth&#039;s &lt;/del&gt;climate &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;system&lt;/del&gt;. It influences atmospheric circulation, weather patterns, and marine ecosystems. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Variations in &lt;/del&gt;global mean SST &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;are indicative of changes in &lt;/del&gt;ocean heat content and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;have implications for phenomena such as El Niño, hurricanes, and long-term climate trends&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;{{SignalTerm|type=DS|id=DS-00002|label=Sea surface temperature (global mean)}} Sea surface temperature (SST) represents the temperature of the ocean&#039;s surface layer and is a &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;fundamental &lt;/ins&gt;parameter in &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the study of &lt;/ins&gt;climate &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and oceanographic processes&lt;/ins&gt;. It influences atmospheric circulation, weather patterns, and marine ecosystems. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Monitoring &lt;/ins&gt;global mean SST &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;provides critical insights into &lt;/ins&gt;ocean heat content and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the Earth&#039;s energy balance&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;The global mean &lt;/del&gt;sea surface temperature &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;integrates measurements from across the world&#039;s oceans&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;providing a comprehensive indicator of oceanic thermal state&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;This parameter &lt;/del&gt;is essential for &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;climate monitoring, oceanographic research, &lt;/del&gt;and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;environmental assessments&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Variations in &lt;/ins&gt;sea surface temperature &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;are linked to phenomena such as El Niño and La Niña, which have widespread climatic impacts. SST changes can affect marine biodiversity, fisheries&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and coral reef health&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Understanding SST trends &lt;/ins&gt;is essential for &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;assessing the responses of the ocean-atmosphere system to natural variability &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;anthropogenic influences&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Changes in SST reflect physical state changes within &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ocean-physical domain, serving &lt;/del&gt;as &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;a key metric for detecting and analyzing &lt;/del&gt;environmental &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;change. Monitoring SST contributes to understanding interactions between &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ocean and atmosphere &lt;/del&gt;and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;supports predictive climate modeling&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;This article describes &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;global mean sea surface temperature &lt;/ins&gt;as &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;an &lt;/ins&gt;environmental &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;signal within &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;SIGNAL Earth observatory system, outlining its measurement, definition, &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;contextual relevance&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Geographic / System Context ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Geographic / System Context ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Sea surface temperature is measured &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;globally &lt;/del&gt;across all ocean basins&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, &lt;/del&gt;including the Atlantic, Pacific, Indian, Southern, and Arctic Oceans. The ocean surface layer&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, typically the upper few meters, &lt;/del&gt;interacts &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;directly &lt;/del&gt;with the atmosphere, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;making SST a boundary condition for air-sea exchanges of heat, moisture&lt;/del&gt;, and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;gases&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Spatial variations &lt;/del&gt;in SST &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;occur due &lt;/del&gt;to &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;factors such as solar radiation, ocean currents, upwelling&lt;/del&gt;, and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;seasonal cycles. The global mean SST aggregates these regional variations to provide an overall state of the ocean surface temperature&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Sea surface temperature is measured across &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the global ocean, encompassing &lt;/ins&gt;all &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;major &lt;/ins&gt;ocean basins including the Atlantic, Pacific, Indian, Southern, and Arctic Oceans. The ocean surface layer interacts with the atmosphere &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and is influenced by regional and global circulation patterns&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;solar radiation&lt;/ins&gt;, and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;heat exchange processes&lt;/ins&gt;. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Variability &lt;/ins&gt;in SST &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;occurs at multiple spatial scales, from local coastal zones &lt;/ins&gt;to &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;basin-wide and global scales&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;reflecting both natural climate variability &lt;/ins&gt;and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;long-term trends&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Monitoring and Measurement ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Monitoring and Measurement ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Monitoring of sea &lt;/del&gt;surface temperature &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;relies on &lt;/del&gt;a combination of satellite remote sensing, in situ &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;observations &lt;/del&gt;from buoys, ships, and floats, and reanalysis products. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Major &lt;/del&gt;monitoring institutions include the National Oceanic and Atmospheric Administration &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;(&lt;/del&gt;NOAA&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;) &lt;/del&gt;and the Copernicus &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Marine Environment Monitoring Service&lt;/del&gt;. Satellite instruments provide &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;broad spatial &lt;/del&gt;coverage &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and high temporal frequency&lt;/del&gt;, while in situ &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;sensors &lt;/del&gt;offer calibration and validation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;data&lt;/del&gt;. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Established datasets &lt;/del&gt;such as the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;NOAA &lt;/del&gt;Optimum Interpolation Sea Surface Temperature (OISST) and the Extended Reconstructed Sea Surface Temperature (ERSST) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;provide continuous and &lt;/del&gt;consistent &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;SST records dating back several decades&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Sea &lt;/ins&gt;surface temperature &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;is monitored through &lt;/ins&gt;a combination of satellite remote sensing, in situ &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;measurements &lt;/ins&gt;from buoys, ships, and floats, and reanalysis products. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Key &lt;/ins&gt;monitoring institutions include the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;[[&lt;/ins&gt;National Oceanic and Atmospheric Administration&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;|&lt;/ins&gt;NOAA&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;]] &lt;/ins&gt;and the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;European Union&#039;s [[&lt;/ins&gt;Copernicus &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Programme|Copernicus]] service&lt;/ins&gt;. Satellite instruments provide &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;high-resolution, near-global &lt;/ins&gt;coverage &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;of SST&lt;/ins&gt;, while in situ &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;data &lt;/ins&gt;offer calibration and validation. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Products &lt;/ins&gt;such as the Optimum Interpolation Sea Surface Temperature (OISST) and the Extended Reconstructed Sea Surface Temperature (ERSST) &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;datasets integrate these observations to produce &lt;/ins&gt;consistent &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;time series for climate analysis&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Within the SIGNAL system, this phenomenon is treated as a defined environmental signal whose boundaries and measurement conventions are described below.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Within the SIGNAL system, this phenomenon is treated as a defined environmental signal whose boundaries and measurement conventions are described below.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Signal Definition ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Signal Definition ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The sea surface temperature (global mean) &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;damage &lt;/del&gt;signal &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;quantifies &lt;/del&gt;the average temperature of the ocean&#039;s surface layer expressed in degrees Celsius (°C). It is derived from the observable type &#039;Sea surface temperature&#039; and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;represents a &lt;/del&gt;state &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;condition within &lt;/del&gt;the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Ocean-Physical domain&lt;/del&gt;. This signal reflects the integrated thermal &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;state &lt;/del&gt;of the &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;global &lt;/del&gt;ocean surface over &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;continuous &lt;/del&gt;time &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;intervals&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;The sea surface temperature (global mean) signal &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;represents &lt;/ins&gt;the average temperature of the ocean&#039;s surface layer&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, &lt;/ins&gt;expressed in degrees Celsius (°C). It is derived from the observable type &#039;Sea surface temperature&#039; and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;quantifies the &lt;/ins&gt;state &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;of &lt;/ins&gt;the &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;ocean&#039;s uppermost thermal environment on a global scale&lt;/ins&gt;. This signal reflects the integrated thermal &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;condition &lt;/ins&gt;of the ocean surface over time &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and space&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Boundary Conditions ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Boundary Conditions ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Boundary inclusions encompass &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;all &lt;/del&gt;measurements of &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;sea surface temperature within &lt;/del&gt;the ocean surface &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;mixed &lt;/del&gt;layer &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;globally&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;including coastal and open &lt;/del&gt;ocean regions. &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Measurements exclude &lt;/del&gt;subsurface &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;temperatures &lt;/del&gt;below the surface layer &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and temperatures from &lt;/del&gt;inland water bodies such as lakes and rivers. The signal &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;does not incorporate &lt;/del&gt;sea ice &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;surface temperatures or land &lt;/del&gt;surface temperatures, focusing solely on &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the &lt;/del&gt;liquid ocean surface.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Boundary inclusions encompass &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the temperature &lt;/ins&gt;measurements of the ocean surface layer, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;typically the upper few millimeters to meters of the &lt;/ins&gt;ocean&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, averaged across all global oceanic &lt;/ins&gt;regions. &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;Boundary exclusions include temperatures from &lt;/ins&gt;subsurface &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;layers &lt;/ins&gt;below the surface &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;skin &lt;/ins&gt;layer&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, &lt;/ins&gt;inland water bodies such as lakes and rivers&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, and coastal land areas&lt;/ins&gt;. The signal &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;excludes atmospheric temperature measurements and &lt;/ins&gt;sea ice surface temperatures, focusing solely on liquid ocean surface &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;waters&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Aggregation Semantics ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Aggregation Semantics ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Geographic aggregation involves averaging sea surface temperature &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;measurements &lt;/del&gt;across the entire global ocean surface, integrating &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;data &lt;/del&gt;from &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;diverse &lt;/del&gt;ocean basins &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and regions&lt;/del&gt;. Temporal aggregation is continuous, with data &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;typically &lt;/del&gt;compiled &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;into &lt;/del&gt;daily, monthly, and annual &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;means &lt;/del&gt;to capture both short-term variability and long-term trends. Cross-signal aggregation &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;considers the relationship of &lt;/del&gt;global mean SST with &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;other &lt;/del&gt;environmental signals such as atmospheric greenhouse gas concentrations and cryosphere &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;metrics, facilitating integrated assessments of &lt;/del&gt;climate system &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;changes&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Geographic aggregation involves averaging sea surface temperature &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;data &lt;/ins&gt;across the entire global ocean surface, integrating &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;measurements &lt;/ins&gt;from &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;all &lt;/ins&gt;ocean basins. Temporal aggregation is continuous, with data compiled &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;and averaged over &lt;/ins&gt;daily, monthly&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;, seasonal&lt;/ins&gt;, and annual &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;intervals &lt;/ins&gt;to capture both short-term variability and long-term trends. Cross-signal aggregation &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;may involve correlating &lt;/ins&gt;global mean SST with &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;related &lt;/ins&gt;environmental signals such as atmospheric greenhouse gas concentrations and cryosphere &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;indicators to assess coupled &lt;/ins&gt;climate system &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;dynamics&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Observational Status ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Observational Status ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Global sea surface temperature is &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;extensively &lt;/del&gt;monitored &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;through multiple, complementary observational platforms, providing robust &lt;/del&gt;datasets &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;with &lt;/del&gt;high &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;spatial and temporal &lt;/del&gt;resolution&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;. Ongoing efforts focus on improving measurement accuracy&lt;/del&gt;, data &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;continuity, and integration of new sensor technologies&lt;/del&gt;. Future SIGNAL releases may &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;incorporate enhanced &lt;/del&gt;spatial &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;granularity&lt;/del&gt;, &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;refined temporal aggregation&lt;/del&gt;, and &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;expanded cross-signal analyses to &lt;/del&gt;support &lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;comprehensive environmental monitoring and research&lt;/del&gt;.&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;Global &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;mean &lt;/ins&gt;sea surface temperature is &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;continuously &lt;/ins&gt;monitored &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;with extensive historical and contemporary &lt;/ins&gt;datasets &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;available. Current products such as NOAA&#039;s OISST provide &lt;/ins&gt;high&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;-&lt;/ins&gt;resolution, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;blended analyses that integrate satellite and in situ &lt;/ins&gt;data. Future SIGNAL releases may &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;enhance temporal and &lt;/ins&gt;spatial &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;resolution&lt;/ins&gt;, &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;incorporate emerging observational platforms&lt;/ins&gt;, and &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;refine uncertainty quantification. Ongoing validation and intercomparison efforts &lt;/ins&gt;support &lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;the reliability of SST data within the SIGNAL framework&lt;/ins&gt;.&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Related Signals ==&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;== Related Signals ==&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l58&quot;&gt;Line 58:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 58:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Ice volume (glaciers)&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Ice volume (glaciers)&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Permafrost ground temperature (borehole)&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Permafrost ground temperature (borehole)&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;−&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;del style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&amp;lt;!-- SIGNAL_EARTH_PEOPLE_START --&amp;gt;&lt;/del&gt;&lt;/div&gt;&lt;/td&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-added&quot;&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;!-- SIGNAL_EARTH_PEOPLE_START --&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;!-- SIGNAL_EARTH_PEOPLE_START --&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Rtuffli</name></author>
	</entry>
	<entry>
		<id>https://wiki.signal-earth.org/index.php?title=Sea_surface_temperature_(global_mean)&amp;diff=32&amp;oldid=prev</id>
		<title>Rtuffli: SIGNAL publish from draft v6</title>
		<link rel="alternate" type="text/html" href="https://wiki.signal-earth.org/index.php?title=Sea_surface_temperature_(global_mean)&amp;diff=32&amp;oldid=prev"/>
		<updated>2026-05-29T17:23:42Z</updated>

		<summary type="html">&lt;p&gt;SIGNAL publish from draft v6&lt;/p&gt;
&lt;table style=&quot;background-color: #fff; color: #202122;&quot; data-mw=&quot;interface&quot;&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;col class=&quot;diff-marker&quot; /&gt;
				&lt;col class=&quot;diff-content&quot; /&gt;
				&lt;tr class=&quot;diff-title&quot; lang=&quot;en&quot;&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;← Older revision&lt;/td&gt;
				&lt;td colspan=&quot;2&quot; style=&quot;background-color: #fff; color: #202122; text-align: center;&quot;&gt;Revision as of 17:23, 29 May 2026&lt;/td&gt;
				&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot; id=&quot;mw-diff-left-l58&quot;&gt;Line 58:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Line 58:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Ice volume (glaciers)&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Ice volume (glaciers)&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Permafrost ground temperature (borehole)&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;* Permafrost ground temperature (borehole)&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-side-deleted&quot;&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot; data-marker=&quot;+&quot;&gt;&lt;/td&gt;&lt;td style=&quot;color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&lt;ins style=&quot;font-weight: bold; text-decoration: none;&quot;&gt;&amp;lt;!-- SIGNAL_EARTH_PEOPLE_START --&amp;gt;&lt;/ins&gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;br&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;!-- SIGNAL_EARTH_PEOPLE_START --&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class=&quot;diff-marker&quot;&gt;&lt;/td&gt;&lt;td style=&quot;background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;&quot;&gt;&lt;div&gt;&amp;lt;!-- SIGNAL_EARTH_PEOPLE_START --&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>Rtuffli</name></author>
	</entry>
	<entry>
		<id>https://wiki.signal-earth.org/index.php?title=Sea_surface_temperature_(global_mean)&amp;diff=30&amp;oldid=prev</id>
		<title>Rtuffli: SIGNAL publish from draft v6</title>
		<link rel="alternate" type="text/html" href="https://wiki.signal-earth.org/index.php?title=Sea_surface_temperature_(global_mean)&amp;diff=30&amp;oldid=prev"/>
		<updated>2026-05-29T17:09:09Z</updated>

		<summary type="html">&lt;p&gt;SIGNAL publish from draft v6&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;&amp;lt;!-- SIGNAL_EARTH_INFOBOX_START --&amp;gt;&lt;br /&gt;
{| class=&amp;quot;wikitable&amp;quot; style=&amp;quot;float:right; clear:right; margin:0 0 1em 1em; width:320px;&amp;quot;&lt;br /&gt;
|+ SIGNAL Earth Structured Data&lt;br /&gt;
|-&lt;br /&gt;
! Object type&lt;br /&gt;
| Damage Signal&lt;br /&gt;
|-&lt;br /&gt;
! SIGNAL Earth ID&lt;br /&gt;
| DS-00002&lt;br /&gt;
|-&lt;br /&gt;
! Observable type&lt;br /&gt;
| Sea surface temperature&lt;br /&gt;
|-&lt;br /&gt;
! Unit&lt;br /&gt;
| °C (degrees Celsius)&lt;br /&gt;
|-&lt;br /&gt;
! Temporal structure&lt;br /&gt;
| Continuous&lt;br /&gt;
|-&lt;br /&gt;
! Monitoring backbone&lt;br /&gt;
| Copernicus / NOAA&lt;br /&gt;
|}&lt;br /&gt;
&amp;lt;!-- SIGNAL_EARTH_INFOBOX_END --&amp;gt;&lt;br /&gt;
&lt;br /&gt;
{{SignalTerm|type=DS|id=DS-00002|label=Sea surface temperature (global mean)}} Sea surface temperature (SST) represents the temperature of the ocean&amp;#039;s surface layer and is a critical parameter in understanding Earth&amp;#039;s climate system. It influences atmospheric circulation, weather patterns, and marine ecosystems. Variations in global mean SST are indicative of changes in ocean heat content and have implications for phenomena such as El Niño, hurricanes, and long-term climate trends.&lt;br /&gt;
&lt;br /&gt;
The global mean sea surface temperature integrates measurements from across the world&amp;#039;s oceans, providing a comprehensive indicator of oceanic thermal state. This parameter is essential for climate monitoring, oceanographic research, and environmental assessments.&lt;br /&gt;
&lt;br /&gt;
Changes in SST reflect physical state changes within the ocean-physical domain, serving as a key metric for detecting and analyzing environmental change. Monitoring SST contributes to understanding interactions between the ocean and atmosphere and supports predictive climate modeling.&lt;br /&gt;
&lt;br /&gt;
== Geographic / System Context ==&lt;br /&gt;
Sea surface temperature is measured globally across all ocean basins, including the Atlantic, Pacific, Indian, Southern, and Arctic Oceans. The ocean surface layer, typically the upper few meters, interacts directly with the atmosphere, making SST a boundary condition for air-sea exchanges of heat, moisture, and gases. Spatial variations in SST occur due to factors such as solar radiation, ocean currents, upwelling, and seasonal cycles. The global mean SST aggregates these regional variations to provide an overall state of the ocean surface temperature.&lt;br /&gt;
&lt;br /&gt;
== Monitoring and Measurement ==&lt;br /&gt;
Monitoring of sea surface temperature relies on a combination of satellite remote sensing, in situ observations from buoys, ships, and floats, and reanalysis products. Major monitoring institutions include the National Oceanic and Atmospheric Administration (NOAA) and the Copernicus Marine Environment Monitoring Service. Satellite instruments provide broad spatial coverage and high temporal frequency, while in situ sensors offer calibration and validation data. Established datasets such as the NOAA Optimum Interpolation Sea Surface Temperature (OISST) and the Extended Reconstructed Sea Surface Temperature (ERSST) provide continuous and consistent SST records dating back several decades.&lt;br /&gt;
&lt;br /&gt;
Within the SIGNAL system, this phenomenon is treated as a defined environmental signal whose boundaries and measurement conventions are described below.&lt;br /&gt;
&lt;br /&gt;
== Signal Definition ==&lt;br /&gt;
The sea surface temperature (global mean) damage signal quantifies the average temperature of the ocean&amp;#039;s surface layer expressed in degrees Celsius (°C). It is derived from the observable type &amp;#039;Sea surface temperature&amp;#039; and represents a state condition within the Ocean-Physical domain. This signal reflects the integrated thermal state of the global ocean surface over continuous time intervals.&lt;br /&gt;
&lt;br /&gt;
== Boundary Conditions ==&lt;br /&gt;
Boundary inclusions encompass all measurements of sea surface temperature within the ocean surface mixed layer globally, including coastal and open ocean regions. Measurements exclude subsurface temperatures below the surface layer and temperatures from inland water bodies such as lakes and rivers. The signal does not incorporate sea ice surface temperatures or land surface temperatures, focusing solely on the liquid ocean surface.&lt;br /&gt;
&lt;br /&gt;
== Aggregation Semantics ==&lt;br /&gt;
Geographic aggregation involves averaging sea surface temperature measurements across the entire global ocean surface, integrating data from diverse ocean basins and regions. Temporal aggregation is continuous, with data typically compiled into daily, monthly, and annual means to capture both short-term variability and long-term trends. Cross-signal aggregation considers the relationship of global mean SST with other environmental signals such as atmospheric greenhouse gas concentrations and cryosphere metrics, facilitating integrated assessments of climate system changes.&lt;br /&gt;
&lt;br /&gt;
== Observational Status ==&lt;br /&gt;
Global sea surface temperature is extensively monitored through multiple, complementary observational platforms, providing robust datasets with high spatial and temporal resolution. Ongoing efforts focus on improving measurement accuracy, data continuity, and integration of new sensor technologies. Future SIGNAL releases may incorporate enhanced spatial granularity, refined temporal aggregation, and expanded cross-signal analyses to support comprehensive environmental monitoring and research.&lt;br /&gt;
&lt;br /&gt;
== Related Signals ==&lt;br /&gt;
* Atmospheric CH4 mole fraction (global)&lt;br /&gt;
* Atmospheric carbon dioxide mole fraction (global mean)&lt;br /&gt;
* Coral reef live cover fraction&lt;br /&gt;
* Dissolved oxygen concentration in coastal waters&lt;br /&gt;
* Glacier area extent&lt;br /&gt;
* Ice sheet mass&lt;br /&gt;
* Ice volume (glaciers)&lt;br /&gt;
* Permafrost ground temperature (borehole)&lt;br /&gt;
&lt;br /&gt;
&amp;lt;!-- SIGNAL_EARTH_PEOPLE_START --&amp;gt;&lt;br /&gt;
== Key Associated People ==&lt;br /&gt;
* &amp;#039;&amp;#039;&amp;#039;Boyin Huang&amp;#039;&amp;#039;&amp;#039; — Contributor (NOAA/NCEI) [Lead author]&lt;br /&gt;
* &amp;#039;&amp;#039;&amp;#039;Kevin S. Casey&amp;#039;&amp;#039;&amp;#039; — Steward-candidate (NASA JPL PO.DAAC) [Dataset owner]&lt;br /&gt;
* &amp;#039;&amp;#039;&amp;#039;Nick A. Rayner&amp;#039;&amp;#039;&amp;#039; — Contributor (Met Office Hadley Centre) [Lead author]&lt;br /&gt;
* &amp;#039;&amp;#039;&amp;#039;Richard W. Reynolds&amp;#039;&amp;#039;&amp;#039; — Advisor (NOAA (historical)) [Lead author]&lt;br /&gt;
&amp;lt;!-- SIGNAL_EARTH_PEOPLE_END --&amp;gt;&lt;br /&gt;
&lt;br /&gt;
&amp;lt;!-- SIGNAL_EARTH_SOURCES_START --&amp;gt;&lt;br /&gt;
== Sources ==&lt;br /&gt;
* {{cite web | title=NOAA NCEI Optimum Interpolation Sea Surface Temperature (OISST) product page | url=https://www.ncei.noaa.gov/products/optimum-interpolation-sst | publisher=NOAA NCEI | year=2026}}&lt;br /&gt;
* {{cite journal | title=Extended Reconstructed Sea Surface Temperature, Version 5 (ERSSTv5): Upgrades, Validations, and Intercomparisons | journal=Journal of Climate | year=2017 | doi=10.1175/JCLI-D-16-0836.1 | url=https://doi.org/10.1175/JCLI-D-16-0836.1}}&lt;br /&gt;
* {{cite journal | title=Daily High-Resolution-Blended Analyses for Sea Surface Temperature | journal=Journal of Climate | year=2007 | doi=10.1175/2007JCLI1824.1 | url=https://doi.org/10.1175/2007JCLI1824.1}}&lt;br /&gt;
* {{cite journal | title=Global analyses of sea surface temperature, sea-ice and night marine air temperature since the late nineteenth century | journal=JGR Atmospheres | year=2003 | doi=10.1029/2002JD002670 | url=https://doi.org/10.1029/2002JD002670}}&lt;br /&gt;
&amp;lt;!-- SIGNAL_EARTH_SOURCES_END --&amp;gt;&lt;/div&gt;</summary>
		<author><name>Rtuffli</name></author>
	</entry>
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