Editing Sea surface temperature

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{| class="wikitable" style="float:right; clear:right; margin:0 0 1em 1em; width:320px;"
|+ SIGNAL Earth Structured Data
|-
! Object type
| Damage Signal
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! SIGNAL Earth ID
| DS-00162
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! Observable type
| Sea surface temperature
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! Unit
| °C (degrees Celsius)
|-
! Temporal structure
| Frequent
|-
! Monitoring backbone
| —
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[https://en.wikipedia.org/wiki/Sea_surface_temperature {{SignalTerm|type=DS|id=DS-00162|label=Sea surface temperature}}] (SST) refers to the temperature of the ocean's surface layer, typically measured within the upper few meters of the water column. It is a fundamental physical parameter influencing atmospheric circulation, marine ecosystems, and climate variability. Variations in SST can affect weather patterns, ocean currents, and biological productivity across the globe.

SST plays a critical role in the exchange of heat and moisture between the ocean and atmosphere, thereby impacting phenomena such as tropical cyclones, monsoons, and El Niño–Southern Oscillation events. Understanding and monitoring SST is essential for climate science, oceanography, and environmental management.

Within the context of global environmental monitoring, sea surface temperature serves as a key indicator of oceanic state changes, reflecting both natural variability and anthropogenic influences. It is widely studied to assess ocean health, climate trends, and the potential for extreme marine events.

== Geographic / System Context ==
Sea surface temperature is a global phenomenon encompassing all ocean basins and marginal seas. It varies spatially due to factors such as latitude, ocean currents, seasonal cycles, and local atmospheric conditions. Equatorial regions generally exhibit higher SSTs, while polar and subpolar regions have lower temperatures. Coastal areas may also experience distinct SST patterns influenced by upwelling, river discharge, and human activities.

The ocean's surface layer interacts dynamically with the atmosphere and marine ecosystems, making SST a central feature of the Earth's climate system. Its global distribution influences regional climates and biogeographic zones within the marine environment.

== Monitoring and Measurement ==
Sea surface temperature is monitored using a combination of satellite remote sensing, in situ measurements from buoys, ships, and autonomous floats, and oceanographic research vessels. Satellite sensors provide frequent, near-global coverage by measuring thermal infrared and microwave emissions from the ocean surface. In situ data are essential for calibration, validation, and capturing subsurface temperature profiles.

Institutions such as the National Oceanic and Atmospheric Administration ([https://en.wikipedia.org/wiki/National_Oceanic_and_Atmospheric_Administration NOAA]), the National Aeronautics and Space Administration ([https://en.wikipedia.org/wiki/NASA NASA]), and international ocean observing programs contribute to the continuous monitoring of SST. Standardized measurement conventions and quality control protocols ensure data reliability and comparability.

Within the SIGNAL system, sea surface temperature is treated as a defined environmental signal whose boundaries and measurement conventions are described below.

== Signal Definition ==
The sea surface temperature signal represents the temperature of the ocean's uppermost layer, expressed in degrees Celsius (°C). It is derived from the Observable Type 'Sea surface temperature' and characterizes the state condition of the ocean domain. This signal captures temporal and spatial variations in SST, reflecting physical changes in ocean surface thermal properties.

== Boundary Conditions ==
Boundary inclusions encompass temperature measurements taken at or near the ocean surface, typically within the upper few meters of the water column, covering all global oceanic and marginal sea areas. Measurements include both open ocean and coastal regions where SST data are available.

Boundary exclusions involve temperature readings from deeper ocean layers below the surface mixed layer, freshwater bodies such as lakes and rivers, and atmospheric temperature measurements. Data affected by ice cover or land contamination are also excluded to maintain signal integrity.

== Aggregation Semantics ==
Geographic aggregation of sea surface temperature data is performed at various spatial scales, ranging from local coastal zones to basin-wide and global averages. Temporal aggregation includes frequent observations aggregated into daily, monthly, seasonal, and annual means to capture short-term variability and long-term trends.

Cross-signal aggregation may involve integrating SST data with related environmental signals such as marine dissolved oxygen concentration and marine heatwave intensity to assess compound oceanographic conditions. Aggregation methods ensure consistency and comparability across datasets and temporal intervals.

== Observational Status ==
Sea surface temperature is extensively monitored with high temporal frequency and global spatial coverage. Existing datasets provide robust baselines for detecting anomalies, trends, and extreme events. Ongoing advancements in satellite technology and in situ observing networks continue to enhance data resolution and accuracy.

Future SIGNAL releases may incorporate improved boundary definitions, refined aggregation methodologies, and integration with complementary oceanographic signals to support comprehensive environmental assessments.

== Related Signals ==
* Marine dissolved oxygen concentration
* Marine heatwave intensity

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== Key Associated People ==
* '''Jens Terhaar''' (University of Bern) [Lead author]
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== Sources ==
* [https://www.nature.com/articles/s41586-025-08674-z Record sea surface temperature jump in 2023–2024 unlikely but not unexpected — 2025]
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