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The dramatic increase of global temperature since the year 2000 has aconsiderable impact on the global water cycle and vegetation dynamics.Little has been done about recent feedback of vegetation to climate indifferent parts of the world, and land evapotranspiration (ET) is the meansof this feedback. Here we used the global 1 km MODIS net primary production (NPP)and ET data sets (2000–2014) to investigate their temporospatialchanges under the context of global warming. The results showed that globalNPP slightly increased in 2000–2014 at a rate of 0.06 PgC yr−2. Morethan 64 % of vegetated land in the Northern Hemisphere (NH) showedincreased NPP (at a rate of 0.13 PgC yr−2), while 60.3 % of vegetatedland in the Southern Hemisphere (SH) showed a decreasing trend (at a rate of−0.18 PgC yr−2). Vegetation greening and climate change promote rises ofglobal ET. Specially, the increased rate of land ET in the NH(0.61 mm yr−2) is faster than that in the SH (0.41 mm yr−2). Over the sameperiod, global warming and vegetation greening accelerate evaporation insoil moisture, thus reducing the amount of soil water storage. Continuationof these trends will likely exacerbate regional drought-induced disturbancesand point to an increased risk of ecological drought, especially duringregional dry climate phases

Dynamic changes in terrestrial net primary production and their effects on evapotranspiration