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

机译:变化气候中洪水频率:加拿大曼尼托巴红河的案例研究

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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:红河流域春季洪水是加拿大曼尼托巴省的经常发生的问题。近年来,已经有许多洪水事件发生了巨大的洪水事件,并提出了气候变化作为潜在的原因。本文采用了一个相对简单的模型,用于预测红河年弹簧峰值排放的频率分布的变化,作为对温室气体浓度的反应。回归模型用于预测前秋季,冬季雪积累和弹簧沉淀中的先前沉淀的弹簧峰流。来自耦合模型离心项目的数据 - 阶段5(CMIP5)用于估计预测器变量的变化,然后采用该信息来导出未来气候条件的洪水分布。大多数气候模型预测冬季的降水量,但这种趋势部分抵消了较短的积雪期和冬季蒸发率更高。 16个气候模型的集合的手段和中位数并不建议更频繁地跨越红河的特定趋势。然而,集合范围比较大,突出了估计极端事件变化所涉及的困难。

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