Multimodel projections and uncertainties of irrigation water demand under climate change

被引:298
作者
Wada, Yoshihide [1 ]
Wisser, Dominik [2 ,3 ]
Eisner, Stephanie [4 ]
Floerke, Martina [4 ]
Gerten, Dieter [5 ]
Haddeland, Ingjerd [6 ]
Hanasaki, Naota [7 ]
Masaki, Yoshimitsu [7 ]
Portmann, Felix T. [8 ,9 ,10 ,11 ]
Stacke, Tobias [12 ]
Tessler, Zachary [13 ]
Schewe, Jacob [5 ]
机构
[1] Univ Utrecht, Dept Phys Geog, NL-3508 TC Utrecht, Netherlands
[2] Univ Bonn, Res Dev Ctr, Bonn, Germany
[3] Univ New Hampshire, Inst Study Earth Oceans & Space, Durham, NH 03824 USA
[4] Univ Kassel, Ctr Environm Syst Res, D-34125 Kassel, Germany
[5] Potsdam Inst Climate Impact Res, Potsdam, Germany
[6] Norwegian Water Resources & Energy Directorate, Oslo, Norway
[7] Natl Inst Environm Studies, Tsukuba, Ibaraki, Japan
[8] Biodivers & Climate Res Ctr LOEWE BiK F, Frankfurt, Germany
[9] Senckenberg Res Inst, Frankfurt, Germany
[10] Nat Hist Museum, Frankfurt, Germany
[11] Goethe Univ Frankfurt, Inst Phys Geog, D-60054 Frankfurt, Germany
[12] Max Planck Inst Meteorol, D-20146 Hamburg, Germany
[13] CUNY City Coll, Environm CrossRoads Initiat, New York, NY 10031 USA
关键词
Irrigation water demand; Climate change; Global hydrological models; CMIP5; Emission scenarios; Uncertainty; INTEGRATED MODEL; SOIL-MOISTURE; SURFACE-WATER; REQUIREMENTS; IMPACTS; RUNOFF; VEGETATION;
D O I
10.1002/grl.50686
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Crop irrigation is responsible for 70% of humanity's water demand. Since the late 1990s, the expansion of irrigated areas has been tapering off, and this trend is expected to continue in the future. Future irrigation water demand (IWD) is, however, subject to large uncertainties due to anticipated climate change. Here, we use a set of seven global hydrological models (GHMs) to quantify the impact of projected global climate change on IWD on currently irrigated areas by the end of this century, and to assess the resulting uncertainties arising from both the GHMs and climate projections. The resulting ensemble projections generally show an increasing trend in future IWD, but the increase varies substantially depending on the degree of global warming and associated regional precipitation changes. Under the highest greenhouse gas emission scenario (RCP8.5), IWD will considerably increase during the summer in the Northern Hemisphere (>20% by 2100), and the present peak IWD is projected to shift one month or more over regions where 80% of the global irrigated areas exist and 4 billion people currently live. Uncertainties arising from GHMs and global climate models (GCMs) are large, with GHM uncertainty dominating throughout the century and with GCM uncertainty substantially increasing from the midcentury, indicating the choice of GHM outweighing by far the uncertainty arising from the choice of GCM and associated emission scenario.
引用
收藏
页码:4626 / 4632
页数:7
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