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The L-band radiometer aboard NASA's Soil Moisture Active Passive (SMAP) platform estimates and analyzes soil moisture and ocean salinity. It detects emitted radiation in the frequency range of 1-2 GHz and have a wavelength range of 30-15 cm. Current space-borne L-band radiometers offer spatial resolutions in the order of 40 km per pixel or 1 km with multi-sensor data fusion algorithms. The sensitivity depth of L-band radiometers offers a trade-off option between thermal imagery and ground penetrating radars for topsoil investigation purposes. Applications of L-band radiometers include investigations into soil moisture and soil variability, sea ice thickness, moisture measurement and leakage detection in structures, and road density changes.

Learn more about near real-time SMAP L-Band Radiometer data provided by NASA's Land, Atmosphere Near real-time Capability for Earth observation (LANCE).

Instrument Type

Spectrometer/Radiometer

Instrument Subtype

Imaging Spectrometer/Radiometer

Specifications

Resolution

Spatial

Soil Moisture: 9 km, 36 km; Sea Surface Salinity depends on processing level: 25 km, 40km, 60 km

Temporal

Soil Moisture: daily; Salinity: 8 days, monthly

Platforms

Frequently Asked Questions

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