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  • IFloodS 2013: A Field Campaign to Support the NASA-JAXA Global Precipitation Measurement Mission x
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Andrea Thorstensen, Phu Nguyen, Kuolin Hsu, and Soroosh Sorooshian

-based observations to retrievals from satellites. The European Space Agency’s Soil Moisture Ocean Salinity (SMOS) satellite mission was launched in 2009 with the purpose of measuring sea surface salinity over the world’s oceans and surface soil moisture over land ( Kerr et al. 2010 ). The recently launched Soil Moisture Active Passive (SMAP) mission from the National Aeronautics and Space Administration (NASA) utilizes a passive L-band radiometer combined with active L-band radar ( Entekhabi et al. 2010

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Evan J. Coopersmith, Michael H. Cosh, Walt A. Petersen, John Prueger, and James J. Niemeier

, 2012 : Validation of Soil Moisture Ocean Salinity (SMOS) soil moisture over watershed networks in the U.S . IEEE Trans. Geosci. Remote Sens. , 50 , 1530 – 1543 , doi: 10.1109/TGRS.2011.2168533 . Jacobs, J. M. , Mohanty B. P. , Hsu E.-C. , and Miller D. , 2004 : SMEX02: Field scale variability, time stability, and similarity of soil moisture . Remote Sens. Environ. , 92 , 436 – 446 , doi: 10.1016/j.rse.2004.02.017 . Joshi, C. , and Mohanty B. P. , 2010 : Physical controls of

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