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Abstract:
Errors in remotely-sensed soil moisture retrievals originate from a
combination of time-invariant and time-varying sources. For land
modeling applications such as forecast initialization, some of the
impact of time-invariant sources can be removed given known
differences between observed and modeled soil moisture climatologies.
Nevertheless, the distinction is seldom made when evaluating
remotely-sensed soil moisture products. Here we describe an Observing
System Simulation Experiment (OSSE) for radiometer-only soil moisture
products from the NASA Hydrosphere States (Hydros) mission where the
impact of time-invariant errors is explicitly removed via the linear
rescaling of retrievals. OSSE results for the 575,000 km2
Red-Arkansas River Basin indicate that climatological rescaling may
significantly reduce the perceived magnitude of Hydros soil moisture
retrieval errors and expand the geographic areas over which retrievals
demonstrate value for land surface modeling applications.