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” (from approximately 1997) particularly affecting southeastern Australia. The Russian heat waves described in Dole et al. (2010) are also reflected in our trends (western Russia), and information from the U.S. Drought Monitor website ( http://droughtmonitor.unl.edu/ ) tends to confirm the decrease in soil moisture observed in the southern United States. The decrease in soil moisture observed in southern South America by ERA-Land and SM-MW (but not by MERRA-Land) is consistent with the negative trends
” (from approximately 1997) particularly affecting southeastern Australia. The Russian heat waves described in Dole et al. (2010) are also reflected in our trends (western Russia), and information from the U.S. Drought Monitor website ( http://droughtmonitor.unl.edu/ ) tends to confirm the decrease in soil moisture observed in the southern United States. The decrease in soil moisture observed in southern South America by ERA-Land and SM-MW (but not by MERRA-Land) is consistent with the negative trends
