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DOI | 10.1007/s00382-018-4314-0 |
Was the North American extreme climate in winter 2013/14 a SST forced response? | |
Peng P.; Kumar A.; Chen M.; Hu Z.-Z.; Jha B. | |
发表日期 | 2019 |
ISSN | 0930-7575 |
起始页码 | 3099 |
结束页码 | 3110 |
卷号 | 52期号:2020-05-06 |
英文摘要 | This study analyzed the possible causes of the atmospheric circulation anomalies responsible for the severe North American (NA) climate in the winter 2013/14. The seasonal (December-January-February) mean circulation anomalies, characterized by an extremely strong ridge off the west coast of NA and an intense trough over the continental US, appeared as a part of wave train across the North Pacific, NA and North Atlantic. The lack of heating-circulation response relationship in the tropics, however, suggested that the wave train might not be a direct response to tropical heating. Meanwhile, dramatic month-to-month variations of the atmospheric circulation over the northeastern Pacific excluded the possibility that the underlying sea surface temperature (SST) anomalies played a dominant role. A further examination of monthly mean circulation patterns suggests that the wave train was initiated by a heating–cooling dipole at the equatorial Pacific in December 2013, and subsequently, was maintained and modified by the extratropical atmospheric internal dynamics in following months. The evolution of tropical heating from December 2013 to February 2014 was associated with the Madden Julian Oscillation (MJO), instead of a quasi-steady response to underlying SST anomalies. Some features of the circulation anomalies in the extratropics for the season can be captured by an atmospheric general circulation model (AGCM) forced with observed SST, but a lack of persistent heating-circulation response relationship in the tropics implied a crucial role of internal variability to extreme NA climate anomalies in the winter 2013/14. © 2018, This is a U.S. government work and its text is not subject to copyright protection in the United States; however, its text may be subject to foreign copyright protection. |
语种 | 英语 |
scopus关键词 | atmospheric circulation; extreme event; general circulation model; heating; Madden-Julian oscillation; sea surface temperature; temperature anomaly; winter; Atlantic Ocean; Atlantic Ocean (North); Pacific Ocean; Pacific Ocean (Equatorial); 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/146480 |
作者单位 | Climate Prediction Center, NCEP/NOAA, 5830 University Research Court, College Park, MD 20740, United States |
推荐引用方式 GB/T 7714 | Peng P.,Kumar A.,Chen M.,et al. Was the North American extreme climate in winter 2013/14 a SST forced response?[J],2019,52(2020-05-06). |
APA | Peng P.,Kumar A.,Chen M.,Hu Z.-Z.,&Jha B..(2019).Was the North American extreme climate in winter 2013/14 a SST forced response?.Climate Dynamics,52(2020-05-06). |
MLA | Peng P.,et al."Was the North American extreme climate in winter 2013/14 a SST forced response?".Climate Dynamics 52.2020-05-06(2019). |
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