Ally M. Toure

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—A microwave radiance assimilation (RA) scheme for the retrieval of snow physical state variables requires a snow-pack physical model (SM) coupled to a radiative transfer model. In order to assimilate microwave brightness temperatures (Tbs) at horizontal polarization (h-pol), an SM capable of resolving melt–refreeze crusts is required. To date, it has not(More)
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