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DOI | 10.1007/s00382-019-04783-4 |
On the weather types that shape the precipitation patterns across the U.S. Midwest | |
Zhang W.; Villarini G. | |
发表日期 | 2019 |
ISSN | 0930-7575 |
起始页码 | 4217 |
结束页码 | 4232 |
卷号 | 53期号:2020-07-08 |
英文摘要 | The U.S. Midwest is an area that has been plagued by heavy and persistent precipitation leading to frequent flood events. The improved understanding of the types of weather conditions and settings associated with heavy precipitation can provide basic information to improve our preparation for and response to these events. Here we identify five weather types from daily 500-hPa geopotential height using the k-means cluster analysis. Consistent with their distinct large-scale atmospheric patterns, these weather types exert different effects on precipitation in the Midwest. Weather type 1 (WT1) features a zonally-aligned wave train propagating from the North Pacific to North America. Overall, WT2 is characterized by a wave train pattern with high (low) pressure in the western (eastern) United States. WT3 features a unique pattern with a high pressure system over the continental United States except for the northwestern United States, similar to the La-Niña forced responses. WT4 is characterized by a wave train moving from the Pacific Northwest to the North Atlantic with a strong ridge over the western United States, while WT5 features a positive geopotential height anomaly originating from the Arctic, probably influenced by the Arctic Amplification. Because of the strong moisture transport, strengthened low-level jet stream and wavy upper-level polar jet stream located in the western United States, among the five weather types WT1 exerts the strongest impacts on precipitation, accounting for up to 40% of the total precipitation over the Midwest, followed by WT5. Moreover, we detect a significant upward trend in the number of WT1 and WT5 events for 1948–2017 and their persistency, suggesting a rising risk of heavy and long-lasting precipitation across the Midwest. Overall, the weather types during summer and winter are consistent with those obtained from the analysis of the entire year, although the weather types during winter have a larger magnitude in the geopotential height anomaly. WT1 accounts for the largest contribution to total precipitation in the Midwest during summer and winter. © 2019, Springer-Verlag GmbH Germany, part of Springer Nature. |
英文关键词 | Precipitation pattern; U.S. Midwest; Weather types |
语种 | 英语 |
scopus关键词 | amplification; climate modeling; cluster analysis; geopotential; jet stream; La Nina; low pressure; numerical model; precipitation (climatology); trend analysis; Midwest; Pacific Ocean; Pacific Ocean (North); United States |
来源期刊 | Climate Dynamics
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/145986 |
作者单位 | IIHR-Hydroscience and Engineering, The University of Iowa, Iowa City, IA, United States |
推荐引用方式 GB/T 7714 | Zhang W.,Villarini G.. On the weather types that shape the precipitation patterns across the U.S. Midwest[J],2019,53(2020-07-08). |
APA | Zhang W.,&Villarini G..(2019).On the weather types that shape the precipitation patterns across the U.S. Midwest.Climate Dynamics,53(2020-07-08). |
MLA | Zhang W.,et al."On the weather types that shape the precipitation patterns across the U.S. Midwest".Climate Dynamics 53.2020-07-08(2019). |
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