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The sea surface skin temperature (SST skin), or ocean skin temperature, is the temperature of the sea surface as determined through its infrared spectrum (3.7–12 μm) and represents the temperature of the sublayer of water at a depth of 10–20 μm. [1]
Sea surface temperature (or ocean surface temperature) is the temperature of ocean water close to the surface. The exact meaning of surface varies in the literature and in practice. It is usually between 1 millimetre (0.04 in) and 20 metres (70 ft) below the sea surface.
The temperature at zero depth is the sea surface temperature. The ocean temperature plays a crucial role in the global climate system, ocean currents and for marine habitats. It varies depending on depth, geographical location and season. Not only does the temperature differ in seawater, so does the salinity.
Sea surface temperature measured in the intake port of large ships have a warm bias of around 0.6 °C (1 °F) due to the heat of the engine room. [25] Since 2000 sea-surface temperatures have increasingly been measured by thermometers on buoys; the apparent cooler temperatures led to an underestimation of global warming since 2000. [ 26 ]
Near-surface air temperature, the temperature of the air near the surface of the Earth; Sea surface temperature, the temperature of water close to the ocean's surface; Global surface temperature, the combined global average of near-surface air temperature and sea surface temperature; Surface temperature of a star, often the effective temperature
Category 1 is a moderate event, Category 2 is a strong event, Category 3 is a severe event, and Category 4 is an extreme event. The category applied to each event in real-time is defined primarily by sea surface temperature anomalies (SSTA), but over time it comes to include typology and characteristics. [25]
This is an example of quality control and monitoring of sea surface temperatures measured by ships and buoys, the iQuam system developed at NOAA/NESDIS/STAR, [3] where statistics show the quality of in situ measurements of sea surface temperatures.
An example is the 2-metre temperature, which is the standard height for near-surface observations of air temperature. This temperature is not directly predicted from the model but is deduced from surface and lowest-model-layer temperatures. Other software is used for creating plots and animations.
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