Reviews of Geophysics · 2012 · 757 citations · 106 references
Natural SciencesEarth SciencesSoil SciencesRemote SensingSoil PhysicsSoil ScienceSatellite Data ValidationSatellite InstrumentationSatellite SensorsSoil MoistureSoil Sensor NetworksSoil VariabilityGround-based ObservationsSatellite ValidationScaling Of Soil MoistureSoil Moisture EstimationSoil Moisture Remote SensingSoil Moisture RetrievalsSoil Moisture ValidationSpatial Variability
Ground‑based soil moisture sensors provide point measurements that are mismatched to the >10 km² satellite footprints, creating sampling uncertainty that can be mistaken for retrieval error and undermine validation accuracy. This review quantifies the upscaling challenge and the required measurement density for ground networks. It also surveys existing upscaling strategies that can mitigate spatial sampling errors in satellite soil moisture validation.
The contrast between the point‐scale nature of current ground‐based soil moisture instrumentation and the ground resolution (typically >10 2 km 2 ) of satellites used to retrieve soil moisture poses a significant challenge for the validation of data products from current and upcoming soil moisture satellite missions. Given typical levels of observed spatial variability in soil moisture fields, this mismatch confounds mission validation goals by introducing significant sampling uncertainty in footprint‐scale soil moisture estimates obtained from sparse ground‐based observations. During validation activities based on comparisons between ground observations and satellite retrievals, this sampling error can be misattributed to retrieval uncertainty and spuriously degrade the perceived accuracy of satellite soil moisture products. This review paper describes the magnitude of the soil moisture upscaling problem and measurement density requirements for ground‐based soil moisture networks. Since many large‐scale networks do not meet these requirements, it also summarizes a number of existing soil moisture upscaling strategies which may reduce the detrimental impact of spatial sampling errors on the reliability of satellite soil moisture validation using spatially sparse ground‐based observations.
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The Soil Moisture Active Passive (SMAP) Mission
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Recent decline in the global land evapotranspiration trend due to limited moisture supply
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