For all regions dominated by long-term TWS depletion, only eastern Brazil (region 6) is collocated with strong nonstationarity in GPP, dominated by a negative trend, reflecting the combined impacts of deforestation, agricultural intensification, and an extended drought ( 35 , 36 , 47 ).
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Nonstationarity in the global terrestrial water cycle and its interlinkages in the Anthropocene.
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The Lower Mississippi (region 5) is the only region where TWS nonstationarity is dominated by a positive trend at a rate of 3 mm/yr.