Anthropogenic influence on multidecadal changes in reconstructed global evapotranspiration

H. Douville (), A. Ribes, B. Decharme, R. Alkama and J. Sheffield
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H. Douville: CNRM-GAME, CNRM/GMGEC/VDR, 42 Avenue G. Coriolis
A. Ribes: CNRM-GAME, CNRM/GMGEC/VDR, 42 Avenue G. Coriolis
B. Decharme: CNRM-GAME, CNRM/GMGEC/VDR, 42 Avenue G. Coriolis
R. Alkama: CNRM-GAME, CNRM/GMGEC/VDR, 42 Avenue G. Coriolis
J. Sheffield: Princeton University

Nature Climate Change, 2013, vol. 3, issue 1, 59-62

Abstract: Understanding the response of evapotranspiration to global warming should help to predict surface climate, including heatwaves and droughts. This study shows that increasing atmospheric concentrations of greenhouse gases and decreasing loadings of anthropogenic (and volcanic) aerosols have led to enhanced evapotranspiration in mid and high latitudes over recent decades.

Date: 2013
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DOI: 10.1038/nclimate1632

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