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Frequency of floods in a changing climate: a case study from the Red River in Manitoba, Canada

机译:气候变化中洪水的发生频率:以加拿大曼尼托巴红河为例

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Spring flooding in the Red River basin is a recurrent issue in the Province of Manitoba, Canada. There have been a number of flood events in recent years and climate change has been suggested as a potential cause. This paper employs a relatively simple model for predicting changes in the frequency distribution of annual spring peak discharge of the Red River as a response to increased GHG concentrations. A regression model is used to predict spring peak flow from antecedent precipitation in the previous fall, winter snow accumulation, and spring precipitation. Data from the Coupled Model Intercomparison Project - Phase 5 (CMIP5) are used to estimate changes in the predictor variables and this information is then employed to derive flood distributions for future climate conditions. Most climate models predict increased precipitation during winter months but this trend is partly offset by a shorter snow accumulation period and higher winter evaporation rates. The means and medians of an ensemble of 16 climate models do not suggest a particular trend toward more or less frequent floods of the Red River. However, the ensemble range is relatively large, highlighting the difficulties involved in estimating changes in extreme events.
机译:红河流域的春季洪水是加拿大曼尼托巴省的一个经常性问题。近年来发生了许多洪水事件,气候变化被认为是潜在的原因。本文采用了一个相对简单的模型来预测红河的年春季峰流量的频率分布变化,以响应增加的温室气体浓度。回归模型用于根据先前秋季的前期降水,冬季积雪和春季降水来预测春季峰值流量。来自耦合模型比较项目-阶段5(CMIP5)的数据用于估计预测变量的变化,然后将该信息用于得出未来气候条件的洪水分布。大多数气候模型预测冬季会出现降水增加,但是这种趋势被较短的积雪期和较高的冬季蒸发率所抵消。 16个气候模型集合的均值和中位数并未显示出红河泛滥的特定趋势。但是,合奏范围相对较大,突显了估算极端事件变化所涉及的困难。

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