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Flood risk in the UK: current and future

机译:英国的洪水风险:当前和未来

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There is a widely-held view that future climate change will increase flood risk in the UK. Extensive modelling studies have been undertaken at CEH to test this hypothesis. The development of continuous river flow simulation techniques for flood frequency estimation now provides a new methodology to predict climate change impacts on flood flows. This technique has been applied to a range of British catchments (work funded by the UK Department for the Environment, Food and Rural Affairs) to assess potential changes in flood risk and directly inform policy development for flood defence scheme appraisal. Using observed climate variables and river flows, the catchment models have been calibrated and validated for the present day. A wide range of climate change scenarios have then been applied to the driving climate data and river flow time series simulated indicative of future time horizons. The flood characteristics of the future have been compared with those of the current. There are many uncertainties associated with this type of climate change impact analysis, including the choice of which Global Climate Model (GCM) to use to derive scenarios of change and precisely how coarse-resolution climate changes (from GCMs) are "downscaled" to the catchment level, as well as hydrological modelling uncertainty. These uncertainties have been assessed, and their effects on the results are discussed. Despite the belief that flood flows will increase in the future, there is no clear message about the size, or even the direction of change in flood flow magnitudes in the UK. Changes in flood flows are catchment-specific, being driven by hydrological variability, such as geology, and the seasonal distribution of rainfall.
机译:有一个广泛的观点认为,未来的气候变化将增加英国的洪水风险。在CEH进行了广泛的建模研究以测试这一假设。用于洪水频率估计的连续河流仿真技术的发展提供了一种新方法,以预测对洪水流动影响的气候变化影响。该技术已应用于一系列英国集水区(由英国环境,食品和农村事务部门资助的工作),以评估洪水风险的潜在变化,直接通知洪水防御计划评估的政策制定。使用观察到的气候变量和河流流动,集水机型已经校准并验证本天。随后已经应用了广泛的气候变化情景,驾驶气候数据和河流流量时间序列模拟指示未来时间视野。将来的洪水特征与目前的洪水特征进行了比较。存在许多与这种类型的气候变化影响分析相关的不确定性,包括选择哪种全球气候模型(GCM)用于推导变革的情景,并准确地是如何粗糙 - 分辨率的气候变化(来自GCMS)是“贬低”集水区水平,以及水文建模不确定性。已经评估了这些不确定性,并讨论了它们对结果的影响。尽管存在洪水流量将来会增加,但对英国的洪水流量大小的变化方向没有明确的信息。洪水流动的变化是集水区的,由水文变异性驱动,如地质和降雨的季节性分布。

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