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Multimodel assessment of water scarcity under climate change

Jacob SchewePotsdam Institute for Climate Impact Research, 14412 Potsdam, Germany;Jens HeinkeInternational Livestock Research Institute, Nairobi, Kenya;Dieter GertenPotsdam Institute for Climate Impact Research, 14412 Potsdam, Germany;Ingjerd HaddelandNorwegian Water Resources and Energy Directorate, N-0301 Oslo, Norway;Nigel W. ArnellWalker Institute for Climate System Research, University of Reading, Reading RG6 6AR, United Kingdom;Douglas B. ClarkCentre for Ecology and Hydrology, Wallingford OX10 8BB, United Kingdom;Rutger DankersMet Office Hadley Centre, Exeter EX1 3PB, United Kingdom;Stephanie EisnerCenter for Environmental Systems Research, University of Kassel, 34109 Kassel, Germany;B M FeketeCivil Engineering Department, The City College of New York, New York, NY 10031;Felipe J. Colón‐GonzálezAbdus Salam International Centre for Theoretical Physics, I-34151Trieste, Italy;Simon N. GoslingSchool of Geography, University of Nottingham, Nottingham NG7 2RD, United Kingdom;Hyungjun KimInstitute of Industrial Science , The University of Tokyo, 4-6-1 Komaba, Meguro, Tokyo 153-8505, Japan;Xingcai LiuInstitute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China;Yoshimitsu MasakiCenter for Global Environmental Research, National Institute for Environmental Studies, Tsukuba 305-8506, Japan;F. T. PortmannInstitute of Physical Geography, Goethe University Frankfurt, 60438 Frankfurt am Main, Germany;Yusuke SatohDepartment of Civil Engineering, The University of Tokyo, 7-3-1 Hongo, Bunkyo, Tokyo 113-8654, Japan;Tobias StackeMax Planck Institute for Meteorology, 20146 Hamburg, Germany;Qiuhong TangInstitute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China;Yoshihide WadaDepartment of Physical Geography, Utrecht University, 3584 CS Utrecht, The Netherlands;Dominik WisserCenter for Development Research, University of Bonn, 53113 Bonn, Germany;Torsten AlbrechtPotsdam Institute for Climate Impact Research, 14412 Potsdam, Germany;Katja FrielerPotsdam Institute for Climate Impact Research, 14412 Potsdam, Germany;Franziska PiontekPotsdam Institute for Climate Impact Research, 14412 Potsdam, Germany;Lila WarszawskiPotsdam Institute for Climate Impact Research, 14412 Potsdam, Germany;P. KabatInternational Institute for Applied Systems Analysis, A-2361 Laxenburg, Austria; and
2013en
ABI

Аннотация

Water scarcity severely impairs food security and economic prosperity in many countries today. Expected future population changes will, in many countries as well as globally, increase the pressure on available water resources. On the supply side, renewable water resources will be affected by projected changes in precipitation patterns, temperature, and other climate variables. Here we use a large ensemble of global hydrological models (GHMs) forced by five global climate models and the latest greenhouse-gas concentration scenarios (Representative Concentration Pathways) to synthesize the current knowledge about climate change impacts on water resources. We show that climate change is likely to exacerbate regional and global water scarcity considerably. In particular, the ensemble average projects that a global warming of 2 °C above present (approximately 2.7 °C above preindustrial) will confront an additional approximate 15% of the global population with a severe decrease in water resources and will increase the number of people living under absolute water scarcity (<500 m(3) per capita per year) by another 40% (according to some models, more than 100%) compared with the effect of population growth alone. For some indicators of moderate impacts, the steepest increase is seen between the present day and 2 °C, whereas indicators of very severe impacts increase unabated beyond 2 °C. At the same time, the study highlights large uncertainties associated with these estimates, with both global climate models and GHMs contributing to the spread. GHM uncertainty is particularly dominant in many regions affected by declining water resources, suggesting a high potential for improved water resource projections through hydrological model development.

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