评估气候模型权重对美国中南部多种方法、变量和领域的敏感性

A. Wootten, E. Massoud, D. Waliser, Huikyo Lee
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引用次数: 2

摘要

摘要鉴于气候预测和多模型集合加权在各种应用中的使用越来越多,该项目评估了气候模型加权策略及其由此产生的综合手段对多个组成部分的敏感性,如加权方案、气候变量或感兴趣的空间域。本研究的目的是评估与多模型加权策略相关的敏感性。该分析利用了耦合模型相互比较项目第五阶段(CMIP5)的全球气候模型及其用局部构造模拟(LOCA)方法创建的统计缩减模型。这项工作的重点是美国中南部的历史和预测未来的月降水量和日高温。结果表明,模型权重和相应的加权模型均值可能对所应用的加权策略敏感。例如,当基于路易西安降水量估计模型权重时,与其他加权策略相比,加权预测显示未来的中南部区域更潮湿、更凉爽。或者,例如,当根据新墨西哥州的温度估计模型权重时,加权预测显示未来中南部地区将更加干燥和温暖。然而,当在估计模型权重时考虑整个资源中心域时,加权的未来预测在降水和温度估计中显示出折衷。至于不确定性,与原始模型样本中的传播相比,我们的结果矩阵提供了一幅更为确定的未来气候图。如果未来的影响评估使用加权策略,那么我们的研究结果表明,具体的加权策略如何与气候预测一起使用可能取决于影响评估或适应计划的需求。
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Assessing sensitivities of climate model weighting to multiple methods, variables, and domains in the south-central United States
Abstract. Given the increasing use of climate projections and multi-model ensemble weighting for a diverse array of applications, this project assesses the sensitivities of climate model weighting strategies and their resulting ensemble means to multiple components, such as the weighting schemes, climate variables, or spatial domains of interest. The purpose of this study is to assess the sensitivities associated with multi-model weighting strategies. The analysis makes use of global climate models from the Coupled Model Intercomparison Project Phase 5 (CMIP5) and their statistically downscaled counterparts created with the localized constructed analogs (LOCA) method. This work focuses on historical and projected future mean precipitation and daily high temperatures of the south-central United States. Results suggest that the model weights and the corresponding weighted model means can be sensitive to the weighting strategy that is applied. For instance, when estimating model weights based on Louisiana precipitation, the weighted projections show a wetter and cooler south-central domain in the future compared to other weighting strategies. Alternatively, for example, when estimating model weights based on New Mexico temperature, the weighted projections show a drier and warmer south-central domain in the future. However, when considering the entire south-central domain in estimating the model weights, the weighted future projections show a compromise in the precipitation and temperature estimates. As for uncertainty, our matrix of results provided a more certain picture of future climate compared to the spread in the original model ensemble. If future impact assessments utilize weighting strategies, then our findings suggest that how the specific weighting strategy is used with climate projections may depend on the needs of an impact assessment or adaptation plan.
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