AI Chat Paper
Note: Please note that the following content is generated by AMiner AI. SciOpen does not take any responsibility related to this content.
{{lang === 'zh_CN' ? '文章概述' : 'Summary'}}
{{lang === 'en_US' ? '中' : 'Eng'}}
Chat more with AI
PDF (30.7 MB)
Collect
Submit Manuscript AI Chat Paper
Show Outline
Outline
Show full outline
Hide outline
Outline
Show full outline
Hide outline
Research Article | Open Access

Water supply‒demand status and management strategies on the Mongolian Plateau

Dong WANGaXian-Hua WEIbXiao-Dong WUa,c( )Tong-Hua WUa,cRen LIa,cGuo-Jie HUa,cDe-Fu ZOUaKe-Yu BAId,eYa-Dong LIUa,cXu-Chun YANa,cXiao-Ying FANa,cAvirmed DASHTSERENfSaruulzaya ADIYAf
Cryosphere Research Station on the Qinghai‒Tibet Plateau, Key Laboratory of Cryospheric Science and Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China
Lanzhou Resource and Environment Vocational and Technical University, Lanzhou 730000, China
University of Chinese Academy Sciences, Beijing 100049, China
Alliance of Bioversity International and International Centre for Tropical Agriculture, Beijing 100081, China
Institute of Agricultural Resources and Regional Planning of Chinese Academy of Agricultural Sciences, Beijing 100081, China
Institute of Geography and Geoecology, Mongolian Academy of Sciences, Ulaanbaatar 15170, Mongolia

Peer review under responsibility of National Climate Centre (China Meteorological Administration)

Show Author Information

Abstract

Arid and semi-arid areas are facing serious water challenges, yet a comprehensive understanding of current and future water supply–demand dynamics remains limited, particularly under climate change and intensified human activities. Based on InVEST and statistical models that include various human activities, we analyzed the patterns and variations of water supply and demand on the Mongolian Plateau for the present period (2001–2020) and projected future (2021–2100). The results showed that grasslands and forests were the primary sources of water supply (77.4%), and cropland was the dominant source of water demand (97.5%), the annual water supply and demand were 238.7 m3/hm2 per year and 546.7 m3/hm2 per year, respectively. From 2001 to 2020, water supply increased by 9.6 m3/hm2 per year (p < 0.01), whereas water demand decreased by 10.5 m3/hm2 per year (p < 0.05). The proportion of areas exhibiting a water surplus increased from 31.5% in 2001 to 51.5% in 2020, primarily due to increased precipitation and a reduction in irrigation water demand. By the end of the 21st century, water supply is projected to increase across all scenarios, ranging from 20.3% to 30.1%, while demand trends diverge: it declines by 28.9%–33.3% under SSP1-2.6, SSP3-7.0, and SSP5-8.5, but rebounds to near-baseline levels under SSP2-4.5. Consequently, water security may improve under SSP1-2.6 and SSP5-8.5 but may deteriorate under SSP2-4.5 and SSP3-7.0. We propose region-specific management strategies, including forest conservation, rotational grazing, irrigation optimization, and inter-basin water allocation. The spatially explicit data and findings provide a valuable foundation for transboundary water cooperation and sustainable dryland water management under a warming climate.

References

【1】
【1】
 
 
Advances in Climate Change Research
Pages 444-456

{{item.num}}

Comments on this article

Go to comment

< Back to all reports

Review Status: {{reviewData.commendedNum}} Commended , {{reviewData.revisionRequiredNum}} Revision Required , {{reviewData.notCommendedNum}} Not Commended Under Peer Review

Review Comment

Close
Close
Cite this article:
WANG D, WEI X-H, WU X-D, et al. Water supply‒demand status and management strategies on the Mongolian Plateau. Advances in Climate Change Research, 2026, 17(2): 444-456. https://doi.org/10.1016/j.accre.2025.12.014

206

Views

1

Downloads

1

Crossref

1

Web of Science

1

Scopus

0

CSCD

Received: 30 May 2025
Revised: 04 December 2025
Accepted: 31 December 2025
Published: 07 January 2026
© 2026

This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).