As part of the preparation for the European Space Agency SMOS (Soil Moisture and Ocean Salinity) ...
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Measuring evaporation (E) with lysimeters is costly and prone to numerous errors. By comparing th...
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A numerical model of the boundary layer of the atmosphere above a gravity surface wave is rev...
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Finer grids in global climate models could lead to an improvement in the simulation of precipitat...
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NRLMSIS® 2.0 is an empirical atmospheric model that extends from the ground to the exobase and de...
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