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过程知情子采样改善了中美洲的次季节降雨预报。

Process-Informed Subsampling Improves Subseasonal Rainfall Forecasts in Central America.

作者信息

Kowal Katherine M, Slater Louise J, Li Sihan, Kelder Timo, Hall Kyle J C, Moulds Simon, García-López Alan A, Birkel Christian

机构信息

Department of Geography and the Environment University of Oxford Oxford UK.

Department of Geography University of Sheffield Sheffield UK.

出版信息

Geophys Res Lett. 2024 Jan 16;51(1):e2023GL105891. doi: 10.1029/2023GL105891. Epub 2024 Jan 5.

DOI:10.1029/2023GL105891
PMID:38993631
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11235057/
Abstract

Subseasonal rainfall forecast skill is critical to support preparedness for hydrometeorological extremes. We assess how a process-informed evaluation, which subsamples forecasting model members based on their ability to represent potential predictors of rainfall, can improve monthly rainfall forecasts within Central America in the following month, using Costa Rica and Guatemala as test cases. We generate a constrained ensemble mean by subsampling 130 members from five dynamic forecasting models in the C3S multimodel ensemble based on their representation of both (a) zonal wind direction and (b) Pacific and Atlantic sea surface temperatures (SSTs), at the time of initialization. Our results show in multiple months and locations increased mean squared error skill by 0.4 and improved detection rates of rainfall extremes. This method is transferrable to other regions driven by slowly-changing processes. Process-informed subsampling is successful because it identifies members that fail to represent the entire rainfall distribution when wind/SST error increases.

摘要

次季节降雨预报技能对于支持应对水文气象极端事件的准备工作至关重要。我们评估了一种基于过程的评估方法,该方法根据预测模型成员表征降雨潜在预测因子的能力对其进行子采样,以哥斯达黎加和危地马拉为测试案例,研究其如何改进中美洲次月的月度降雨预报。我们通过在初始化时基于(a)纬向风向以及(b)太平洋和大西洋海表温度(SST)的表征,从C3S多模型集合中的五个动态预测模型的130个成员中进行子采样,生成一个受限集合平均值。我们的结果表明,在多个月份和地点,均方误差技能提高了0.4,极端降雨的检测率也有所提高。该方法可转移到由缓慢变化过程驱动的其他地区。基于过程的子采样之所以成功,是因为它识别出当风/SST误差增加时未能表征整个降雨分布的成员。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0b39/11235057/1955c92ffe58/GRL-51-e2023GL105891-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0b39/11235057/ea4992e4882e/GRL-51-e2023GL105891-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0b39/11235057/a1a4a8b6221a/GRL-51-e2023GL105891-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0b39/11235057/0e5c100d64b7/GRL-51-e2023GL105891-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0b39/11235057/1955c92ffe58/GRL-51-e2023GL105891-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0b39/11235057/ea4992e4882e/GRL-51-e2023GL105891-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0b39/11235057/a1a4a8b6221a/GRL-51-e2023GL105891-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0b39/11235057/0e5c100d64b7/GRL-51-e2023GL105891-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0b39/11235057/1955c92ffe58/GRL-51-e2023GL105891-g002.jpg

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