Antecedent snowmelt and orographic precipitation contributions to water supply of Pakistan disastrous floods, 2022

IF 6.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES
Yan Wang , Peng Cui , Chen-Di Zhang , Guo-Tao Zhang , Jian-Sheng Hao , Xu Yuan , Yao-Zhi Jiang , Lu Wang
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Abstract

In 2022, the Pakistan witnessed the hottest spring and wettest summer in history. And devastating floods inundated a large portion of Pakistan and caused enormous damages. However, the primary water source and its contributions to these unprecedented floods remain unclear. Based on the reservoir inflow measurements, Multi-Source Weighted-Ensemble Precipitation (MSWEP), the fifth generation ECMWF atmospheric reanalysis (ERA5) products, this study quantified the contributions of monsoon precipitation, antecedent snowmelts, and orographic precipitation enhancement to floods in Pakistan. We found that the Indus experienced at least four inflow uprushes, which was mainly supplied by precipitation and snowmelt; In upper Indus, abnormally high temperature continued to influence the whole summer and lead to large amounts of snowmelts which not only was a key water supply to the flood but also provided favorable soil moisture conditions for the latter precipitation. Before July, the snowmelt has higher contributions than the precipitation to the streamflow of Indus River, with contribution value of more than 60%. Moreover, the snowmelt could still supply 20%–40% water to the lower Indus in July and August; The leading driver of 2022 mega-floods over the southern Pakistan in July and August was dominated by the precipitation, where terrain disturbance induced precipitation account to approximately 33% over the southern Pakistan. The results help to understand the mechanisms of flood formation, and to better predict future flood risks over complex terrain regions.

2022 年巴基斯坦灾难性洪水的前期融雪和地貌降水对供水的贡献
2022 年,巴基斯坦经历了历史上最炎热的春季和最潮湿的夏季。毁灭性的洪水淹没了巴基斯坦大部分地区,造成了巨大损失。然而,这些史无前例的洪水的主要水源及其贡献仍不清楚。本研究基于水库流入量测量、多源加权集合降水(MSWEP)和第五代 ECMWF 大气再分析(ERA5)产品,量化了季风降水、先期降雪和地貌降水增强对巴基斯坦洪水的贡献。我们发现,印度河至少经历了四次洪水暴涨,主要由降水和融雪提供;在印度河上游,异常高温持续影响了整个夏季,导致大量融雪,这不仅是洪水的关键水源,也为后一次降水提供了有利的土壤水分条件。7 月以前,融雪对印度河流量的贡献率高于降水,贡献值超过 60%。此外,在 7 月和 8 月,融雪仍可为印度河下游提供 20%-40% 的水量;7 月和 8 月,巴基斯坦南部地区 2022 年特大洪水的主要驱动因素是降水,其中地形扰动引起的降水在巴基斯坦南部地区约占 33%。这些结果有助于了解洪水形成的机制,更好地预测复杂地形区未来的洪水风险。
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来源期刊
Advances in Climate Change Research
Advances in Climate Change Research Earth and Planetary Sciences-Atmospheric Science
CiteScore
9.80
自引率
4.10%
发文量
424
审稿时长
107 days
期刊介绍: Advances in Climate Change Research publishes scientific research and analyses on climate change and the interactions of climate change with society. This journal encompasses basic science and economic, social, and policy research, including studies on mitigation and adaptation to climate change. Advances in Climate Change Research attempts to promote research in climate change and provide an impetus for the application of research achievements in numerous aspects, such as socioeconomic sustainable development, responses to the adaptation and mitigation of climate change, diplomatic negotiations of climate and environment policies, and the protection and exploitation of natural resources.
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