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首页> 外文期刊>Natural Hazards and Earth System Sciences Discussions >Spatio-temporal evolution of wet–dry event features and their transition across the Upper Jhelum Basin (UJB) in South Asia
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Spatio-temporal evolution of wet–dry event features and their transition across the Upper Jhelum Basin (UJB) in South Asia

机译:湿干事件特征的时空演变及其在南亚上部jhelum盆地(UJB)的过渡

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摘要

The increasing rate of occurrence of extreme events (droughts and floods)and their rapid transition magnify the associated socio-economic impactswith respect to those caused by the individual event. Understanding ofspatio-temporal evolution of wet–dry events collectively, theircharacteristics, and the transition (wet to dry and dry to wet) is thereforesignificant to identify and locate most vulnerable hotspots, providing thebasis for the adaptation and mitigation measures. The Upper Jhelum Basin(UJB) in South Asia was selected as a case study, where the relevance ofwet–dry events and their transition has not been assessed yet, despiteclear evidence of climate change in the region. The standardizedprecipitation evapotranspiration index (SPEI) at the monthly timescale wasapplied to detect and characterize wet and dry events for the period1981–2014. The results of temporal variations in SPEI showed a strong changein basin climatic features associated with El Ni?o–Southern Oscillation(ENSO) at the end of 1997, with the prevalence of wet and dry events beforeand after 1997 respectively. The results of spatial analysis show a highersusceptibility of the monsoon-dominated region towards wet events, with moreintense events occurring in the eastern part, whereas a higher severity andduration are featured in the southwestern part of the basin. In contrast, thewesterlies-dominated region was found to be the hotspot of dry events withhigher duration, severity, and intensity. Moreover, the surrounding regionof the Himalaya divide line and the monsoon-dominated part of the basin werefound to be the hotspots of rapid wet–dry transition events.
机译:越来越多的极端事件(干旱和洪水)及其快速转变的速度倍数放大了各个事件引起的相关的社会经济撞击声。了解湿干事件的空行演化,它们是共同的,它们的特征和过渡(湿到干燥和干燥到湿),无法识别和定位最脆弱的热点,为适应和缓解措施提供基础。南亚的上部Jhelum盆地(UJB)被选为案例研究,其中尚未评估WET-DREVENT事件及其过渡的相关性,绝​​抗在该地区气候变化的证据。标准化的预科蒸发蒸发指数(SPEI)在每月时间措施被捕获,以检测和表征周期1981-2014的潮湿和干燥事件。 Spei的时间变化结果表明,1997年底与EL NI?O-Southern振荡(ENSO)相关的强大变化盆地气候功能,分别在1997年之后的湿法和干燥事件盛行的患病率。空间分析结果表明,季风占主导地区对潮湿事件的升高性,在东部发生的温度发生,而盆地的西南部是更高的严重程度。相比之下,发现临时占主导地位的地区是具有高度,严重程度和强度的干事件的热点。此外,喜马拉雅划分线和盆地的季风主导部分的周围地区被捕,是快速湿润过渡事件的热点。

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