Projected Changes in SWA over the Main BRI Regions for Net-Zero and Net-Negative Future

Author:

He Jing12ORCID,Zhang Jingyong34,Dong Wenjie12,Zhuang Yuanhuang5

Affiliation:

1. School of Atmospheric Sciences, Sun Yat-sen University & Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, 519082, China.

2. Key Laboratory of Tropical Atmosphere-Ocean System, Ministry of Education, Sun Yat-sen University, Zhuhai, 519082, China.

3. Center for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China.

4. College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, 100049, China.

5. Tianjin Meteorological Observatory, Tianjin, 300000, China.

Abstract

Surface water availability (SWA, calculated by precipitation [P] minus actual evaporation [E]) has great impacts on society. However, it remains unclear how SWA will change in a net-zero and net-negative future. In this study, we examine future changes in P, E, and SWA from the Coupled Model Intercomparison Project Phase 6 (CMIP6) for net-zero (2050–2060) and net-negative (2090–2100) CO 2 emissions periods under pathway SSP1-1.9 relative to historical baseline (1995–2014) in the main Belt and Road Initiative (BRI) regions. We also consider SSP2-4.5 and SSP5-8.5 for comparison. We find that P, E, and SWA changes exhibit obvious spatial heterogeneity, with increase or decrease over different areas for 2050–2060 and 2090–2100 relative to 1995–2014 under 3 scenarios. SWA changes are generally insignificant excluding some isolated areas under SSP1-1.9, yet have statistical significances over Central Africa and many areas in Eurasia for SSP2-4.5 and SSP5-8.5. Average monthly P and E are expected to markedly increase by 2.63 and 2.01 mm, 1.85 and 1.65 mm, for net-zero and net-negative periods under SSP1-1.9. Consequently, the projected monthly SWA will change by 0.78 and 0.36 mm. However, the projected P, E, and SWA have much larger changes in the same periods under the other 2 scenarios, especially 2090–2100. Our research provides previously unknown knowledge that SWA shows quite different changes in the net-zero and net-negative periods under SSP1-1.9 relative to the same periods under SSP2-4.5 and SSP5-8.5, which may facilitate management of water resource risks to ecosystems and human society.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Management, Monitoring, Policy and Law,Ecology,Ecology, Evolution, Behavior and Systematics

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