Increasing Drought Risks Over the Past Four Centuries Amidst Projected Flood Intensification in the Kabul River Basin (Afghanistan and Pakistan)-Evidence From Tree Rings

被引:12
作者
Khan, Nasrullah [1 ,2 ]
Nguyen, Hung T. T. [3 ]
Galelli, Stefano [4 ,5 ]
Cherubini, Paolo [2 ,3 ,5 ]
机构
[1] Univ Malakand, Dept Bot, Chakdara, Pakistan
[2] WSL Swiss Fed Inst Forest Snow & Landscape Res, Birmensdorf, Switzerland
[3] Columbia Univ, Lamont Doherty Earth Observ, Tree Ring Lab, Palisades, NY 10964 USA
[4] Singapore Univ Technol & Design, Pillar Engn Syst & Design, Singapore, Singapore
[5] Univ British Columbia, Fac Forestry, Vancouver, BC, Canada
基金
瑞士国家科学基金会;
关键词
dendrochronology; precipitation reconstruction; drought; climate change; water resources; water cycle; KARAKORAM TEMPERATURE; NORTHERN PAKISTAN; INDUS BASIN; CLIMATE; RECONSTRUCTION; MECHANISMS; MANAGEMENT; TRENDS; CYCLE;
D O I
10.1029/2022GL100703
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Increased flood risks have been projected, but with large uncertainties, in the Kabul River Basin (Afghanistan and Pakistan). To place future changes in a long-term perspective, we produce a 382-year precipitation reconstruction for the basin using seven tree-ring chronologies of old-growth conifers from the Hindu Kush Mountains, a monsoon-shadow area. The reconstruction proves robust over rigorous cross-validations (R-2 = 0.60, RE = 0.60, CE = 0.53). The full reconstruction (1637-2018) reveals a steady decline in the low end of the precipitation distribution, implying increasing drought risks. We show that droughts are getting more severe, shorter, and more frequent, interspersed with more frequent pluvials in the past century. Drought risks, compounded with projected flood intensification, pose significant threats for this transboundary river. Therefore, future water management needs to account for both flood and drought risks and be informed by long-term hydroclimatic variability.
引用
收藏
页数:11
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