SMAP underestimates soil moisture in vegetation-disturbed areas primarily as a result of biased surface temperature data

Author:

Fan XingwangORCID,Liu Yuanbo,Gan GuojingORCID,Wu Guiping

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Computers in Earth Sciences,Geology,Soil Science

Reference51 articles.

1. The global SMOS Level 3 daily soil moisture and brightness temperature maps;Al Bitar;Earth Syst. Sci. Data,2017

2. NASA/GSFC/HSL, GLDAS Noah Land Surface Model L4 3 hourly 0.25 x 0.25 degree V2.1;Beaudoing,2020

3. Assessment of the SMAP passive soil moisture product;Chan;IEEE T. Geosci. Remote,2016

4. Global land precipitation: a 50-yr monthly analysis based on gauge observations;Chen;J. Hydrometeorol.,2002

5. Effect of surface roughness on the microwave emission from soils;Choudhury;J. Geophys. Res.-Oceans,1979

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