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首页> 外文期刊>Journal of Hydrology >Assessing the impacts of climate change on river flows in England using the UKCP09 climate change projections
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Assessing the impacts of climate change on river flows in England using the UKCP09 climate change projections

机译:使用UKCP09气候变化预测评估气候变化对英格兰河流流量的影响

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This paper presents an assessment of the effects of climate change on river flow regimes in representative English catchments, using the UKCP09 climate projections. These comprise a set of 10,000 coherent climate scenarios, used here (i) to evaluate the distribution of potential changes in hydrological behaviour and (ii) to construct relationships between indicators of climate change and hydrological change. The study uses six catchments, and focuses on change in average flow, high flow (Q5) and low flow (Q95). There is a large range in hydrological change in each catchment between the plausible UKCP09 climate projections, with differences between catchments largely due to differences in catchment geology and baseline water balance. The range in change between the UKCP09 projections is in most catchments smaller than the range between changes with scenarios based on the CMIP3 ensemble of climate models (although the shape of the distribution of changes is different), and earlier UK scenarios produce changes that tend towards the lower (drier) end of the UKCP09 range. The difference between emissions scenarios is small compared to the range across the 10,000 scenarios. Changes in high flows are largely driven by changes in winter precipitation, whilst changes in low flows are determined by changes in summer precipitation and temperature. (C) 2014 Elsevier B.V. All rights reserved.
机译:本文利用UKCP09气候预测,对英国代表流域气候变化对河流流量状况的影响进行了评估。这些构成了10,000个相关的气候情景的集合,在这里用于(i)评估水文行为潜在变化的分布,以及(ii)构造气候变化指标与水文变化之间的关系。该研究使用了六个流域,重点研究了平均流量,高流量(Q5)和低流量(Q95)的变化。在合理的UKCP09气候预测之间,每个流域的水文变化范围很大,流域之间的差异主要是由于流域地质和基线水平衡的差异。在大多数流域,UKCP09预测之间的变化范围小于基于气候模型CMIP3集合的情景变化之间的幅度(尽管变化的分布形式有所不同),而早期的英国情景所产生的变化倾向于UKCP09范围的较低(较干燥)端。与10,000个方案的排放范围相比,排放方案之间的差异很小。高流量的变化主要由冬季降水的变化驱动,而低流量的变化由夏季降水和温度的变化确定。 (C)2014 Elsevier B.V.保留所有权利。

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