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Global terrestrial water storage and drought severity under climate change

Urheber*innen

Pokhrel,  Yadu
External Organizations;

Felfelani,  Farshid
External Organizations;

Satoh,  Yusuke
External Organizations;

Boulange,  Julien
External Organizations;

Burek,  Peter
External Organizations;

/persons/resource/Anne.Gaedeke

Gädeke,  Anne
Potsdam Institute for Climate Impact Research;

/persons/resource/Dieter.Gerten

Gerten,  Dieter
Potsdam Institute for Climate Impact Research;

Gosling,  Simon N.
External Organizations;

Grillakis,  Manolis
External Organizations;

Gudmundsson,  Lukas
External Organizations;

Hanasaki,  Naota
External Organizations;

Kim,  Hyungjun
External Organizations;

Koutroulis,  Aristeidis
External Organizations;

Liu,  Junguo
External Organizations;

Papadimitriou,  Lamprini
External Organizations;

/persons/resource/Schewe

Schewe,  Jacob
Potsdam Institute for Climate Impact Research;

Müller Schmied,  Hannes
External Organizations;

Stacke,  Tobias
External Organizations;

Telteu,  Camelia-Eliza
External Organizations;

Thiery,  Wim
External Organizations;

Veldkamp,  Ted
External Organizations;

Zhao,  Fang
External Organizations;

Wada,  Yoshihide
External Organizations;

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Zitation

Pokhrel, Y., Felfelani, F., Satoh, Y., Boulange, J., Burek, P., Gädeke, A., Gerten, D., Gosling, S. N., Grillakis, M., Gudmundsson, L., Hanasaki, N., Kim, H., Koutroulis, A., Liu, J., Papadimitriou, L., Schewe, J., Müller Schmied, H., Stacke, T., Telteu, C.-E., Thiery, W., Veldkamp, T., Zhao, F., Wada, Y. (2021): Global terrestrial water storage and drought severity under climate change. - Nature Climate Change, 11, 3, 226-233.
https://doi.org/10.1038/s41558-020-00972-w


Zitierlink: https://publications.pik-potsdam.de/pubman/item/item_25181
Zusammenfassung
Terrestrial water storage (TWS) modulates the hydrological cycle and is a key determinant of water availability and an indicator of drought. While historical TWS variations have been increasingly studied, future changes in TWS and the linkages to droughts remain unexamined. Here, using ensemble hydrological simulations, we show that climate change could reduce TWS in many regions, especially those in the Southern Hemisphere. Strong inter-ensemble agreement indicates high confidence in the projected changes that are driven primarily by climate forcing rather than land and water management activities. Declines in TWS translate to increases in future droughts. By the late twenty-first century, the global land area and population in extreme-to-exceptional TWS drought could more than double, each increasing from 3% during 1976–2005 to 7% and 8%, respectively. Our findings highlight the importance of climate change mitigation to avoid adverse TWS impacts and increased droughts, and the need for improved water resource management and adaptation.