Climate Change Data Portal
DOI | 10.1007/s00382-018-4223-2 |
Dynamical analysis of extreme precipitation in the US northeast based on large-scale meteorological patterns | |
Agel L.; Barlow M.; Colby F.; Binder H.; Catto J.L.; Hoell A.; Cohen J. | |
发表日期 | 2019 |
ISSN | 0930-7575 |
起始页码 | 1739 |
结束页码 | 1760 |
卷号 | 52期号:2020-03-04 |
英文摘要 | Previous work has identified six large-scale meteorological patterns (LSMPs) of dynamic tropopause height associated with extreme precipitation over the Northeast US, with extreme precipitation defined as the top 1% of daily station precipitation. Here, we examine the three-dimensional structure of the tropopause LSMPs in terms of circulation and factors relevant to precipitation, including moisture, stability, and synoptic mechanisms associated with lifting. Within each pattern, the link between the different factors and extreme precipitation is further investigated by comparing the relative strength of the factors between days with and without the occurrence of extreme precipitation. The six tropopause LSMPs include two ridge patterns, two eastern US troughs, and two troughs centered over the Ohio Valley, with a strong seasonality associated with each pattern. Extreme precipitation in the ridge patterns is associated with both convective mechanisms (instability combined with moisture transport from the Great Lakes and Western Atlantic) and synoptic forcing related to Great Lakes storm tracks and embedded shortwaves. Extreme precipitation associated with eastern US troughs involves intense southerly moisture transport and strong quasi-geostrophic forcing of vertical velocity. Ohio Valley troughs are associated with warm fronts and intense warm conveyor belts that deliver large amounts of moisture ahead of storms, but little direct quasi-geostrophic forcing. Factors that show the largest difference between days with and without extreme precipitation include integrated moisture transport, low-level moisture convergence, warm conveyor belts, and quasi-geostrophic forcing, with the relative importance varying between patterns. © 2018, Springer-Verlag GmbH Germany, part of Springer Nature. |
语种 | 英语 |
scopus关键词 | atmospheric circulation; atmospheric dynamics; extreme event; geostrophic flow; precipitation assessment; seasonal variation; three-dimensional modeling; United States |
来源期刊 | Climate Dynamics |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/146556 |
作者单位 | Department of Environmental, Earth, and Atmospheric Sciences, University of Massachusetts Lowell, One University Avenue, Lowell, MA, United States; Intercampus Marine Science Graduate Program, University of Massachusetts Lowell, Lowell, MA, United States; Climate Change Initiative, University of Massachusetts Lowell, Lowell, MA, United States; Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland; Laboratoire de Météorologie Dynamique/IPSL, École Normale Supérieure, Paris, France; College of Engineering, Mathematics and Physical Sciences, University of Exeter, Exeter, United Kingdom; NOAA/ESRL Physical Sciences Division, Boulder, CO, United States; Atmospheric and Environmental Research, Lexington, MA, United States |
推荐引用方式 GB/T 7714 | Agel L.,Barlow M.,Colby F.,et al. Dynamical analysis of extreme precipitation in the US northeast based on large-scale meteorological patterns[J],2019,52(2020-03-04). |
APA | Agel L..,Barlow M..,Colby F..,Binder H..,Catto J.L..,...&Cohen J..(2019).Dynamical analysis of extreme precipitation in the US northeast based on large-scale meteorological patterns.Climate Dynamics,52(2020-03-04). |
MLA | Agel L.,et al."Dynamical analysis of extreme precipitation in the US northeast based on large-scale meteorological patterns".Climate Dynamics 52.2020-03-04(2019). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。