Generated by GPT-5-mini| SMAP (satellite) | |
|---|---|
| Name | SMAP |
| Mission type | Earth observation |
| Operator | National Aeronautics and Space Administration (NASA) |
| COSPAR ID | 2015-001A |
| SATCAT | 40304 |
| Manufacturer | Jet Propulsion Laboratory / Northrop Grumman |
| Launch mass | 924 kg |
| Power | 2,000 W |
| Launch date | January 31, 2015 |
| Launch vehicle | Delta II |
| Launch site | Vandenberg Air Force Base |
| Orbit reference | Geocentric orbit |
| Orbit regime | Sun-synchronous orbit |
| Orbit altitude | 685 km |
| Instrument type | Radiometer, Radar (synthetic aperture) |
SMAP (satellite)
SMAP is a NASA Earth observation satellite designed to measure global soil moisture and freeze–thaw state using a combined L-band radiometer and radar payload. Developed by Jet Propulsion Laboratory and launched from Vandenberg Air Force Base on a Delta II rocket, SMAP provides high-resolution, frequent global maps to support research and applications across hydrology, climatology, ecology, and agriculture. The mission supports operational agencies such as the United States Department of Agriculture, National Oceanic and Atmospheric Administration, and international partners including the European Space Agency and Canadian Space Agency.
SMAP was conceived under NASA's Earth System Science Pathfinder program with project management at Jet Propulsion Laboratory and instrument procurement involving Northrop Grumman. Its primary objective was to deliver frequent, global measurements of surface soil moisture and landscape freeze–thaw state to improve predictions within weather forecasting models, river discharge estimates, and carbon cycle assessments. The mission addressed recommendations from panels convened by National Research Council (United States) and contributed to international efforts coordinated by the Global Climate Observing System. SMAP's design emphasized a wide-swath, L-band sensor suite to balance spatial resolution, temporal revisit, and sensitivity over terrestrial and coastal environments.
The SMAP spacecraft carried a deployable 6-meter rotating reflector supporting an L-band passive radiometer and an active synthetic-aperture radar built to operate near 1.4 GHz. Major subsystems were provided by Northrop Grumman and flight operations were conducted by teams at Jet Propulsion Laboratory and NASA's Goddard Space Flight Center. The radiometer used a conical-scanning feed to produce brightness temperature measurements, while the radar transmitted pulses to measure backscatter for surface scattering and roughness. Ancillary systems included GPS receivers for precise orbit determination, star trackers and reaction wheels for attitude control, and a phased antenna feed to support combined radar-radiometer data fusion. Thermal control was managed with radiators and insulation in collaboration with instrument teams from University of Michigan and other academic partners.
SMAP's science objectives focused on three primary targets: global surface soil moisture mapping, freeze–thaw state detection, and the derivation of higher-level products for hydrology and carbon cycle science. Measurements combined L-band brightness temperature and radar backscatter to estimate near-surface soil moisture within the top ~5 cm and to detect freeze–thaw transitions that influence net ecosystem exchange of carbon dioxide. Data products supported assimilation into land-surface models used by European Centre for Medium-Range Weather Forecasts, National Weather Service, and research models at institutions such as Columbia University and Princeton University. Validation campaigns involved field sites managed by United States Geological Survey, regional networks like FLUXNET, and international observatories coordinated through Global Soil Moisture Data Bank initiatives.
SMAP was launched on January 31, 2015 aboard a Delta II rocket from Vandenberg Air Force Base into a sun-synchronous afternoon equator-crossing orbit. Post-launch commissioning included deployment of the 6-meter reflector and calibration of radiometer and radar channels, with mission operations run by teams at Jet Propulsion Laboratory and ground services supported by the White Sands Complex and other ground stations. Following an early anomaly that affected the radar instrument, NASA adjusted the mission plan to continue operations using radiometer-only and combined-processing approaches; operations involved mission planning, onboard health monitoring, and routine calibration using targets such as Amazon Rainforest, Sahara Desert, and polar sites. SMAP operated within international coordination frameworks including data sharing arrangements with European Space Agency missions like Soil Moisture and Ocean Salinity.
SMAP data were processed through a hierarchy of levels from calibrated brightness temperatures to geophysical products for soil moisture and freeze–thaw state. Processing pipelines were implemented at Jet Propulsion Laboratory and distributed via NASA's National Snow and Ice Data Center and NASA Earthdata portals, with ancillary datasets drawn from MODIS, Landsat, Sentinel-1, and reanalyses from ECMWF. Product suites included Level 2 and Level 3 soil moisture, freeze–thaw maps, and Level 4 model-assimilated fields suitable for use by operational centers such as National Weather Service and by researchers at Woods Hole Oceanographic Institution and University of California, Berkeley. Data formats followed community standards used by Committee on Earth Observation Satellites and were accompanied by validation reports from networks including International Soil Moisture Network.
SMAP produced the first global, high-resolution maps of near-surface soil moisture and freeze–thaw state with frequent revisit, enabling advances in flood forecasting, drought monitoring, and carbon flux estimation. Results demonstrated improved river runoff predictions in studies with USGS hydrologists, enhanced agricultural water-management decision support used by United States Department of Agriculture, and refined carbon exchange estimates in boreal regions studied by teams at University of Alaska Fairbanks and Yale University. The mission spurred methodological developments in data assimilation exploited by NASA Global Modeling and Assimilation Office and fostered international collaborations with European Space Agency and Canadian Space Agency. SMAP legacy activities continue through follow-on missions, algorithm refinements at institutions like Caltech and Massachusetts Institute of Technology, and incorporation of SMAP products into operational services provided by agencies such as NOAA.
Category:Earth observation satellites Category:NASA satellites Category:2015 in spaceflight