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DOI | 10.5194/hess-24-5125-2020 |
Rivers in the sky; flooding on the ground: The role of atmospheric rivers in inland flooding in central Europe | |
Ionita M.; Nagavciuc V.; Guan B. | |
发表日期 | 2020 |
ISSN | 1027-5606 |
起始页码 | 5125 |
结束页码 | 5147 |
卷号 | 24期号:11 |
英文摘要 | The role of large-scale atmospheric circulation and atmospheric rivers (ARs) in producing extreme flooding and heavy rainfall events in the lower part of the Rhine catchment area is examined in this study. Analysis of the largest 10 floods in the lower Rhine, between 1817 and 2015, shows that all these extreme flood peaks have been preceded up to 7 d in advance by intense moisture transport from the tropical North Atlantic basin in the form of narrow bands also known as atmospheric rivers. Most of the ARs associated with these flood events are embedded in the trailing fronts of the extratropical cyclones. The typical large-scale atmospheric circulation leading to heavy rainfall and flooding in the lower Rhine is characterized by a low pressure center south of Greenland, which migrates toward Europe, and a stable high pressure center over the northern part of Africa and the southern part of Europe and projects on the positive phase of the North Atlantic Oscillation. On the days preceding the flood peaks, lower (upper) level convergence (divergence) is observed over the analyzed region, which indicates strong vertical motions and heavy rainfall. Vertically integrated water vapor transport (IVT) exceeds 600 kgm-1 s-1 for the largest floods, marking these as very strong ARs. The results presented in this study offer new insights regarding the importance of moisture transport as a driver of extreme flooding in the lower part of the Rhine catchment area, and we show, for the first time, that ARs are a useful tool for the identification of potentially damaging floods in inland Europe. © Author(s) 2020. |
语种 | 英语 |
scopus关键词 | Atmospheric movements; Atmospheric pressure; Catchments; Climatology; Flood control; Moisture; Rain; Rivers; Runoff; Storms; Atmospheric circulation; Catchment area; Extratropical cyclones; Inland flooding; Integrated water vapors; Moisture transport; North Atlantic oscillations; Vertical motions; Floods; atmospheric circulation; catchment; flood; flood damage; flood deposit; flooding; high pressure; low pressure; North Atlantic Oscillation; rainfall; spatiotemporal analysis; water vapor; Africa; Arctic; Atlantic Ocean; Atlantic Ocean (North); Europe; Greenland; Rhine River |
来源期刊 | Hydrology and Earth System Sciences
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/159273 |
作者单位 | Ionita, M., Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany; Nagavciuc, V., Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany, Faculty of Forestry, Štefan Cel Mare University, Suceava, Romania; Guan, B., Joint Institute for Regional Earth System Science and Engineering, University of California, Los Angeles, CA, United States, Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, United States |
推荐引用方式 GB/T 7714 | Ionita M.,Nagavciuc V.,Guan B.. Rivers in the sky; flooding on the ground: The role of atmospheric rivers in inland flooding in central Europe[J],2020,24(11). |
APA | Ionita M.,Nagavciuc V.,&Guan B..(2020).Rivers in the sky; flooding on the ground: The role of atmospheric rivers in inland flooding in central Europe.Hydrology and Earth System Sciences,24(11). |
MLA | Ionita M.,et al."Rivers in the sky; flooding on the ground: The role of atmospheric rivers in inland flooding in central Europe".Hydrology and Earth System Sciences 24.11(2020). |
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