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Fig. 20.4 ( a ) Landsat Thematic Mapper NDII and VWC for corn and soybeans during the Soil
Moisture Experiments ( SMEX ) 2002 and 2005 in Ames, Iowa (Yilmaz et al. 2008b ). ( b )A
comparison between VWC estimated from MODIS and WindSat (circular footprint of 25-km
radius) for agricultural areas in central Iowa 2003-2005 (Hunt et al. 2011b )
their stomata (Jones 2007 ; Passioura 2007 ; Waring and Landsberg 2011 ), which
decreases latent heat loss and increases canopy temperatures detectable in the thermal
infrared (Anderson et al. 2003 ; Kustas and Anderson 2009 ). Some species avoid
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