Himawari, covering eastern Asia and Oceaniaĭata is processed and fused into a global product, covering most of the globe's land surface within the -60°/70° latitude range at a spatial resolution of 5°/112.Geostationary Operational Environmental Satellite (GOES East), covering North and South America.Meteosat Second Generation Indian Ocean Data Coverage (IODC) covering the Middle East.Meteosat Second Generation (MSG) 0°, covering Europe and Africa.The Copernicus LST datasets are obtained from a constellation of geostationary (GEO) satellites: LST10-TCI: Thermal Condition Index with a 10-day composite of Land Surface Temperature.LST10-DC: 10-day Land Surface Temperature with Daily Cycle.LST: hourly LST from instantaneous observations. The Global Land Service provides the following LST-based products: In turn, the LST influences the partition of energy between ground and vegetation, and determines the surface air temperature. Because both respond rapidly to changes in incoming solar radiation due to cloud cover and aerosol load modifications and diurnal variation of illumination, the LST displays quick variations too. LST is a mixture of vegetation and bare soil temperatures. Its estimation further depends on the albedo, the vegetation cover and the soil moisture. It is estimated from Top-of-Atmosphere brightness temperatures from the infrared spectral channels of a constellation of geostationary satellites (Meteosat Second Generation, GOES, MTSAT/Himawari). The Land Surface Temperature (LST) is the radiative skin temperature of the land surface, as measured in the direction of the remote sensor.
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