ESA’s Soil Moisture and Ocean Salinity (SMOS) Earth Explorer mission was launched on November 2, 2009 to observe two important components of the water cycle. Its L-band interferometric radiometer measures microwave brightness temperature, from which soil moisture over land and sea-surface salinity over oceans are retrieved. These products support studies of surface–atmosphere exchange, weather and climate, with additional applications to thin sea ice. Soil-moisture and salinity products have different spatial and temporal averaging requirements: ESA describes roughly 50 km soil-moisture mapping every three days, while high-precision salinity estimates use substantially broader spatial and multi-day averaging. The retrievals require product-specific interpretation rather than treating brightness temperature as moisture or salinity directly.
Schedule, status, and mission updates. Time-based alerts will start when a time is available.
ESA’s Soil Moisture and Ocean Salinity (SMOS) Earth Explorer mission was launched on November 2, 2009 to observe two important components of the water cycle. Its L-band interferometric radiometer measures microwave brightness temperature, from which soil moisture over land and sea-surface salinity over oceans are retrieved. These products support studies of surface–atmosphere exchange, weather and climate, with additional applications to thin sea ice. Soil-moisture and salinity products have different spatial and temporal averaging requirements: ESA describes roughly 50 km soil-moisture mapping every three days, while high-precision salinity estimates use substantially broader spatial and multi-day averaging. The retrievals require product-specific interpretation rather than treating brightness temperature as moisture or salinity directly.
Schedule, status, and mission updates. Time-based alerts will start when a time is available.