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Long-term precipitation trends and climate extremes in the Kelani River basin, Sri Lanka, and their impact on streamflow variability under climate change

机译:Kelani River河流域,斯里兰卡的长期降水趋势和气候极值及其对气候变化下的流出变异性的影响

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This paper focuses on and analyses the potential hydrological impacts of climate change on the hydrologic regime of the Kelani River basin, Sri Lanka. In this research, future basin-wide hydrology is simulated by using downscaled temperature and precipitation outputs from the Canadian Earth System Model, version 2 (CanESM2), and the Hydrologic Engineering Centre's Hydrologic Modeling System (HEC-HMS). The research further evaluates the long-term behavior and trends of climate extremes based on observed historical temperature and precipitation data. The findings suggest that temperature and precipitation extremes are on the rise while the annual average precipitation in the basin is declining. It is also predicted with the application of statistical downscaling that temperature may rise annually for representative concentration pathways of RCP2.6, RCP4.5, and RCP8.5. A detailed modeling approach is applied to the Hanwella sub-watershed (1799.67km(2)) of the Kelani River basin to study subsequent water resource management options required to ensure the sustainable development alternatives with varying streamflow in the Kelani River basin under the effects of future (2020s, 2050s, and 2080s) rainfall and temperature as impending climate change becomes manifested. This paper reviews the current state of the catchment as well as the suitability of applying GCMs rather than RCMs to Sri Lanka to assess this river basin, according to monthly, seasonal, and annual variations of the climatology. Further, a quantitative analysis of the change of amount of surface water in the selected river basin with respect to the expected variations in precipitation and temperature is also carried out. The findings of this research and overall outcome will be useful in identifying possible climate change impact on paddy and crop production, ensuing sustainable water management scenarios, best management options, and mitigation measures in land use, carbon emission management, etc., in a more meaningful manner in the future. This study will set the baseline for commencing and continuing quantitative studies incorporating the behavior of the basin-wide climatology and streamflow variability with the use of GCMs to achieve sustainable development goals.
机译:本文重点介绍并分析了气候变化对斯里兰卡的克拉尼河流域水文制度的潜在水文影响。在这项研究中,通过使用来自加拿大地球系统模型,版本2(CANESM2)和水文工程中心的水文建模系统(HEC-HMS)的次要温度和降水输出来模拟未来的流域水文。该研究进一步评估了基于观察到的历史温度和降水数据的气候极值的长期行为和趋势。研究结果表明,极端的温度和降水量正在上升,而盆地的年平均降水正在下降。还预测统计较透露的统计缩小的应用,该温度可能每年上升,用于RCP2.6,RCP4.5和RCP8.5的代表性浓度途径。将采用详细的建模方法应用于Kelani River盆地的Hanwella子流域(1799.67公里(2)),以研究随后的水资源管理方案,以确保在Kelani River盆地的影响下,在Kelani River盆地的效果下实现可持续发展的替代方案未来(2020年代,2050年代和2080年代)降雨量和温度随着即将发生的气候变化而变得表现出来。本文评论了该集水区的现状,以及适用于将GCMS而不是RCMS应用于斯里兰卡,以评估这条河流域,根据月季度,季节性和年度变化的气候学。此外,还进行了相对于沉淀和温度的预期变化的所选河流盆中表面水量变化的定量分析。本研究和整体结果的调查结果可用于确定可能的气候变化对稻谷和作物生产的影响,随之而来的可持续水管理场景,最佳管理选择和降低土地利用,碳排放管理等的缓解措施。未来有意义的方式。本研究将设定开始和持续的定量研究的基线,这些研究纳入流域气候学的行为,并利用GCMS实现可持续发展目标的流出变异性。

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