Southern Hemisphere dominates recent decline in global water availability

Author:

Zhang Yongqiang1ORCID,Li Congcong23ORCID,Chiew Francis H. S.3ORCID,Post David A.3ORCID,Zhang Xuanze1ORCID,Ma Ning1ORCID,Tian Jing1ORCID,Kong Dongdong4ORCID,Leung L. Ruby5ORCID,Yu Qiang2ORCID,Shi Jiancheng6ORCID,Liu Changming1

Affiliation:

1. Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China.

2. State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, China.

3. CSIRO Environment, Black Mountain, Canberra, ACT 2601, Australia.

4. Department of Atmospheric Science, School of Environmental Studies, China University of Geosciences, Wuhan, China.

5. Pacific Northwest National Laboratory, Richland, WA 99352, USA.

6. National Space Science Center, Chinese Academy of Sciences, Beijing 100190, China.

Abstract

Global land water underpins livelihoods, socioeconomic development, and ecosystems. It remains unclear how water availability has changed in recent decades. Using an ensemble of observations, we quantified global land water availability over the past two decades. We show that the Southern Hemisphere has dominated the declining trend in global water availability from 2001 to 2020. The significant decrease occurs mainly in South America, southwestern Africa, and northwestern Australia. In the Northern Hemisphere, the complex regional increasing and decreasing trends cancel each other, resulting in a negligible hemispheric trend. The variability and trend in water availability in the Southern Hemisphere are largely driven by precipitation associated with climate modes, particularly the El Niño-Southern Oscillation. This study highlights their dominant role in controlling global water availability.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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