Impact of Climate Change on Flood Factors and Extent of Damages in the Hindu Kush Region

A. Rahman, Shakeel Mahmood, Mohammad H. Dawood, G. Rahman, Fang Chen
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引用次数: 6

Abstract

This chapter analyzes the impacts of climate change on flood factors and extent of associated damages in the Hindu Kush (HK) region. HK mountains system is located in the west of the Himalayas and Karakorum. It is the greatest watershed of the River Kabul, River Chitral, River Panjkora, and River Swat in the eastern Hindu Kush and River Amu in western Hindu Kush. The Hindu Kush system hosts numerous glaciers, snow-clad mountains, and fertile river valleys; it also supports large populations and provides year-round water to recharge streams and rivers. The study region is vulnerable to a wide range of hazards including floods, earthquakes, landslides, desertification, and drought. Flash floods and riverine floods are the deadliest extreme hydro-meteorological events. The upper reaches experience characteristics of flash flooding, whereas the lower reach is where river floods occur. Flash floods are more destructive and sudden. Almost every year in summer, monsoonal rainfall and high temperature join hands with heavy melting of glaciers and snow accelerating discharge in the river system. In the face of climate change, a significant correlation between rainfall patterns, trends in temperature, and resultant peaks in river discharge have been recorded. A rising trend was found in temperature, which leads to early and rapid melting of glaciers and snow in the headwater region. The analysis reveals that during the past three decades, radical changes in the behavior of numerous valley glaciers have been noted. In addition, the spatial and temporal scales of violent weather events have been growing, since the 1980s. Such changes in water regimes including the frequent but substantial increase in heavy precipitation events and rapid melting of snow in the headwater region, siltation in active channels, excessive deforestation, and human encroachments onto the active flood channel have further escalated the flooding events. The HK region is beyond the reach of existing weather RADAR network, and hence forecasting and early warning is ineffective. Here, almost every year, the floods cause damages to infrastructure, scarce farmland, and sources of livelihood.
气候变化对兴都库什地区洪水因素及损失程度的影响
本章分析了气候变化对兴都库什山(香港)地区洪水因素和相关损害程度的影响。香港山系位于喜马拉雅山脉和喀喇昆仑山脉的西部。它是东部兴都库什山脉的喀布尔河、吉德拉尔河、潘杰科拉河、斯瓦特河和西部兴都库什山脉的阿姆河的最大分水岭。兴都库什山脉拥有众多的冰川、冰雪覆盖的山脉和肥沃的河谷;它还支持大量人口,并提供全年的水来补充溪流和河流。研究区域容易受到洪水、地震、滑坡、荒漠化和干旱等多种灾害的影响。山洪和河流洪水是最致命的极端水文气象事件。上游具有山洪暴发的特征,而下游则是河流洪水发生的地方。山洪更具破坏性和突发性。几乎每年夏季,季风性降雨和高温加上冰川和积雪的大量融化,加速了河流系统的排放。面对气候变化,降雨模式、温度趋势和由此产生的河流流量峰值之间存在显著的相关性。气温有上升的趋势,导致源区冰川和积雪的早期和快速融化。分析表明,在过去三十年中,已经注意到许多山谷冰川的行为发生了根本变化。此外,自20世纪80年代以来,暴力天气事件的时空尺度一直在增长。这些水势的变化,包括频繁但大量增加的强降水事件和源头地区快速的积雪融化,活跃渠道的淤积,过度的森林砍伐和人类对活跃洪道的侵占,进一步加剧了洪水事件。香港地区不在现有天气雷达网络的覆盖范围内,因此预报和预警是无效的。在这里,几乎每年都有洪水对基础设施、稀缺的农田和生计来源造成破坏。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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