Editing Sea surface salinity

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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-00167
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! Observable type
| Sea surface salinity
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! Unit
| PSU (PSU)
|-
! Temporal structure
| Monthly
|-
! Monitoring backbone
| —
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{{SignalTerm|type=DS|id=DS-00167|label=Sea surface salinity}} (SSS) refers to the concentration of dissolved salts in the uppermost layer of the ocean, typically measured in practical salinity units (PSU). It is a fundamental property influencing ocean circulation, climate variability, and marine ecosystems. Variations in sea surface salinity reflect changes in the water cycle, including evaporation, precipitation, river discharge, and ice melting.

Understanding sea surface salinity patterns is essential for interpreting ocean-atmosphere interactions and the global hydrological cycle. It also plays a critical role in modulating sea surface density, which drives thermohaline circulation and affects climate systems on regional and global scales.

Recent research indicates that global-scale patterns of sea surface salinity have intensified since the late 19th century, highlighting the importance of long-term monitoring to detect state changes in ocean salinity and their environmental implications.

== Geographic / System Context ==
Sea surface salinity is a global oceanographic parameter, measured across all major ocean basins including the Atlantic, Pacific, Indian, Southern, and Arctic Oceans. Spatial variability in salinity is influenced by geographic factors such as latitude, proximity to freshwater sources, and prevailing climate regimes. For example, higher salinities are typically observed in subtropical regions due to elevated evaporation rates, while lower salinities occur near river outflows and polar ice melt zones. The distribution of sea surface salinity is interconnected with large-scale ocean circulation patterns and regional climatic phenomena such as monsoons and El Niño-Southern Oscillation.

== Monitoring and Measurement ==
Sea surface salinity is monitored using a combination of in situ and remote sensing methods. In situ observations are obtained from research vessels, moored buoys, and autonomous floats such as those deployed in the Argo program. These measurements provide direct, high-accuracy salinity profiles near the ocean surface. Satellite missions, including the Soil Moisture and Ocean Salinity (SMOS) and Aquarius satellites, offer global coverage by measuring microwave emissions related to surface salinity. Data from these sources are integrated and calibrated to produce monthly global salinity maps, facilitating the analysis of temporal and spatial trends.

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

== Signal Definition ==
The {{SignalTerm|type=DS|id=DS-00167|label=Sea surface salinity}} Damage Signal represents the state condition of dissolved salt concentration at the ocean surface, quantified in practical salinity units (PSU). It captures monthly averaged salinity values reflecting the physical state of the ocean's uppermost layer, serving as an indicator of oceanic and climatic processes influencing salinity distribution.

== Boundary Conditions ==
Boundary inclusions encompass all ocean surface waters globally, including coastal zones and open ocean regions where salinity measurements are feasible. The signal excludes subsurface salinity layers below the immediate sea surface, freshwater bodies such as lakes and rivers, and terrestrial environments. Measurements are confined to the upper ocean layer typically influenced by atmospheric and hydrological processes, excluding deep ocean salinity variations.

== Aggregation Semantics ==
Geographic aggregation of sea surface salinity data is performed at multiple spatial scales, ranging from localized coastal areas to basin-wide and global ocean regions. Temporal aggregation follows a monthly cadence to capture seasonal and interannual variability while smoothing short-term fluctuations. Cross-signal aggregation may integrate sea surface salinity with related environmental signals such as [https://en.wikipedia.org/wiki/Sea_surface_temperature sea surface temperature] and coastal salinity intrusion extent to assess combined impacts on marine and climate systems. Aggregation methods prioritize consistent spatial grids and temporal intervals to facilitate comparative analyses and trend detection.

== Observational Status ==
Current monitoring of sea surface salinity leverages a growing network of satellite sensors and in situ platforms, providing increasingly comprehensive global coverage and temporal resolution. Data assimilation efforts continue to improve the accuracy and consistency of salinity products. Future SIGNAL releases may incorporate enhanced datasets with finer spatial resolution, expanded temporal records, and integration with complementary oceanographic variables to support more detailed assessments of salinity dynamics and their environmental consequences.

== Related Signals ==
* Coastal salinity intrusion extent

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== Key Associated People ==
* '''W. John Gould''' (National Oceanography Centre) [Lead author]
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== Sources ==
* [https://www.nature.com/articles/s43247-021-00161-3 Global-scale patterns of observed sea surface salinity intensified since the 1870s — 2021]
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