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Hydrology of mountainous areas in the upper Indus Basin,Northern Pakistan with the perspective of climate change

机译:气候变化视角下的巴基斯坦北部印度河上游山区水文学

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Mountainous areas in the northern Pakistan are blessed by numerous rivers that have great potential in water resources and hydropower production. Many of these rivers are unexploited for their water resource potential. If the potential of these rivers are explored, hydropower production and water supplies in these areas may be improved. The Indus is the main river originating from mountainous area of the Himalayas of Baltistan, Pakistan in which most of the smaller streams drain. In this paper, the hydrology of the mountainous areas in northern Pakistan is studied to estimate flow pattern, long-term trend in river flows, characteristics of the watersheds, and variability in flow and water resource due to impact of climate change. Eight watersheds including Gilgit, Hunza, Shigar, Shyok, Astore, Jhelum, Swat, and Chitral, Pakistan have been studied from 1960 to 2005 to monitor hydrological changes in relation to variability in precipitation, temperature and mean monthly flows, trend of snow melt runoff, analysis of daily hydrographs, water yield and runoff relationship, and flow duration curves. Precipitation from ten meteorological stations in mountainous area of northern Pakistan showed variability in the winter and summer rains and did not indicate a uniform distribution of rains. Review of mean monthly temperature of ten stations suggested that the Upper Indus Basin can be categorized into three hydrological regimes, i.e., high-altitude catchments with large glacierized parts, middle-altitude catchments south of Karakoram, and foothill catchments. Analysis of daily runoff data (1960-2005) of eight watersheds indicated nearly a uniform pattern with much of the runoff in summer (June-August). Impact of climate change on long-term recorded annual runoff of eight watersheds showed fair water flows at the Hunza and Jhelum Rivers while rest of the rivers indicated increased trends in runoff volumes. The study of the water yield availability indicated a minimum trend in Shyok River at Yogo and a maximum trend in Swat River at Kalam. Long-term recorded data used to estimate flow duration curves have shown a uniform trend and are important for hydropower generation for Pakistan which is seriously facing power crisis in last 5 years.
机译:巴基斯坦北部山区拥有众多河流,这些河流在水资源和水力发电方面具有巨大潜力。这些河流中有许多由于其水资源潜力而未被开发。如果挖掘这些河流的潜力,这些地区的水力发电和供水将得到改善。印度河是源自巴基斯坦巴尔的斯坦喜马拉雅山山区的主要河流,大部分较小的河流都流向印度河。本文研究了巴基斯坦北部山区的水文状况,以估算流量模式,河流流量的长期趋势,流域特征以及由于气候变化而造成的流量和水资源的变化。从1960年到2005年,对包括吉尔吉特(Gilgit),洪扎(Hunza),希加尔(Shigar),夏洛克(Shyok),阿斯托(Astore),杰鲁姆(Jhelum),斯瓦特(Swat)和巴基斯坦奇特拉尔(Chitral)在内的八个流域进行了研究,以监测与降水量,温度和平均月流量,融雪径流趋势有关的水文变化。 ,每日水文图分析,水产量与径流关系以及水流持续时间曲线。巴基斯坦北部山区十个气象站的降水显示,冬季和夏季降雨变化多端,并且未表明降雨分布均匀。回顾十个测站的月平均温度,可以将印度河上游地区划分为三个水文情势,即具有较大冰川部分的高海拔集水区,喀喇昆仑山脉以南的中海拔集水区和山麓集水区。对八个流域的每日径流数据(1960-2005年)进行的分析表明,夏季(6月至8月)的大部分径流几乎是均匀的。气候变化对八个流域长期记录的年度径流的影响表明,洪扎河和杰勒姆河的水流公平,而其余河流表明径流量增加。对可用水量的研究表明,Yogo的Shyok河出现了最小趋势,Kalam的Swat河出现了最大趋势。用于估计流量持续时间曲线的长期记录数据显示出一个统一的趋势,对于巴基斯坦的水力发电非常重要,因为巴基斯坦在过去5年中正面临着严重的电力危机。

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