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The Effect of Multi-Model Averaging of Climate Model Outputs on the Seasonality of Rainfall Over the Columbia River Basin

机译:气候模式输出多模型平均对哥伦比亚河流域降水季节性的影响

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摘要

The rainfall seasonality index is the measure of precipitation distribution throughout the seasonal cycle. The aim of this study is to compare the effect of different multi-model averaging methods on the rainfall seasonality index at each 1/16 latitude-longitude cells covering the Columbia River Basin. In accordance with the same, ten different climate model outputs are selected from 45 available climate models from CMIP5 dataset. The reanalysis precipitation data is used to estimate the errors in rainfall seasonality for the climate model outputs. The inverse variance method and statistical multi criteria analysis (SMCA) method were used to estimate the weights for each climate model output. The precipitation amounts from the climate model outputs were then averaged using these model weights. The rainfall seasonality index was estimated from: (1) observed reanalysis data; (2) averaged precipitation amount from ten combinations of CMIP5 outputs for the current climate (1979–2005) using inverse variance method; (3) averaged precipitation amount from the ten combinations of CMIP5 outputs for the current climate using SMCA. The results showed the large differences in rainfall seasonality index for each climate model averaging. Moreover, the multi-modelling of climate models resulted in relative improvements in the performance of the rainfall seasonality over the Columbia River Basin. The estimated model weights for the current climate can be useful to combine the model outputs for the future climate.
机译:降雨季节指数是整个季节周期内降雨分布的量度。本研究的目的是比较覆盖哥伦比亚河流域的每个1/16纬度-经度单元上不同的多模型平均方法对降雨季节指数的影响。同样,从CMIP5数据集中的45种可用气候模型中选择了十种不同的气候模型输出。重新分析降水数据用于估算气候模型输出的降雨季节性误差。使用逆方差法和统计多准则分析(SMCA)方法估算每个气候模型输出的权重。然后使用这些模型权重对气候模型输出的降水量进行平均。降雨季节指数从以下方面估算:(1)观测到的再分析数据; (2)使用逆方差法从当前气候(1979–2005)的十种CMIP5输出组合中获得的平均降水量; (3)使用SMCA从当前气候的CMIP5输出的十个组合中得出的平均降水量。结果表明,每种气候模式平均值的降雨季节性指数差异很大。此外,气候模型的多模型化导致哥伦比亚河流域降雨季节性表现的相对改善。当前气候的估计模型权重可能有助于合并未来气候的模型输出。

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