Improving terrestrial evaporation estimates over continental Australia through assimilation of SMOS soil moisture
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文摘

Modelled surface soil moisture from GLEAM can be improved through the assimilation of SMOS soil moisture.

The effect of the assimilation of satellite soil moisture on the modelled evaporation is mild and not definitive.

SMOS soil moisture appears to have a higher quality compared to AMSR-E soil moisture over continental Australia.

The quality of the descending AMSR-E data is notably higher compared to the ascending data.

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