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DOI | 10.1007/s00382-019-05004-8 |
Maximizing ENSO as a source of western US hydroclimate predictability | |
Patricola C.M.; O’Brien J.P.; Risser M.D.; Rhoades A.M.; O’Brien T.A.; Ullrich P.A.; Stone D.A.; Collins W.D. | |
发表日期 | 2020 |
ISSN | 0930-7575 |
起始页码 | 351 |
结束页码 | 372 |
卷号 | 54期号:2020-01-02 |
英文摘要 | Until recently, the El Niño–Southern Oscillation (ENSO) was considered a reliable source of winter precipitation predictability in the western US, with a historically strong link between extreme El Niño events and extremely wet seasons. However, the 2015–2016 El Niño challenged our understanding of the ENSO-precipitation relationship. California precipitation was near-average during the 2015–2016 El Niño, which was characterized by warm sea surface temperature (SST) anomalies of similar magnitude compared to the extreme 1997–1998 and 1982–1983 El Niño events. We demonstrate that this precipitation response can be explained by El Niño’s spatial pattern, rather than internal atmospheric variability. In addition, observations and large-ensembles of regional and global climate model simulations indicate that extremes in seasonal and daily precipitation during strong El Niño events are better explained using the ENSO Longitude Index (ELI), which captures the diversity of ENSO’s spatial patterns in a single metric, compared to the traditional Niño3.4 index, which measures SST anomalies in a fixed region and therefore fails to capture ENSO diversity. The physically-based ELI better explains western US precipitation variability because it tracks the zonal shifts in tropical Pacific deep convection that drive teleconnections through the response in the extratropical wave-train, integrated vapor transport, and atmospheric rivers. This research provides evidence that ELI improves the value of ENSO as a predictor of California’s seasonal hydroclimate extremes compared to traditional ENSO indices, especially during strong El Niño events. © 2019, The Author(s). |
英文关键词 | ENSO; Extreme events; Hydroclimate; Precipitation; Predictability; Western US |
语种 | 英语 |
scopus关键词 | air-sea interaction; climate modeling; climate prediction; El Nino-Southern Oscillation; extreme event; precipitation (climatology); sea surface temperature; temperature anomaly; vapor pressure; California; Pacific Ocean; Pacific Ocean (Tropical); 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/145760 |
作者单位 | Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA, United States; Department of Earth and Planetary Sciences, University of California, Santa Cruz, Santa Cruz, CA, United States; Department of Land, Air and Water Resources, University of California, Davis, Davis, CA, United States; Global Climate Adaptation Partnership, Oxford, United Kingdom; Computational Research Division, Lawrence Berkeley National Laboratory, Berkeley, CA, United States; Department of Earth and Planetary Science, University of California, Berkeley, Berkeley, CA, United States |
推荐引用方式 GB/T 7714 | Patricola C.M.,O’Brien J.P.,Risser M.D.,et al. Maximizing ENSO as a source of western US hydroclimate predictability[J],2020,54(2020-01-02). |
APA | Patricola C.M..,O’Brien J.P..,Risser M.D..,Rhoades A.M..,O’Brien T.A..,...&Collins W.D..(2020).Maximizing ENSO as a source of western US hydroclimate predictability.Climate Dynamics,54(2020-01-02). |
MLA | Patricola C.M.,et al."Maximizing ENSO as a source of western US hydroclimate predictability".Climate Dynamics 54.2020-01-02(2020). |
条目包含的文件 | 条目无相关文件。 |
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