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DOI | 10.1002/wcc.527 |
Equatorial Atlantic variability—Modes, mechanisms, and global teleconnections | |
Lübbecke J.F.; Rodríguez-Fonseca B.; Richter I.; Martín-Rey M.; Losada T.; Polo I.; Keenlyside N.S. | |
发表日期 | 2018 |
ISSN | 1757-7780 |
EISSN | 1757-7779 |
卷号 | 9期号:4 |
英文摘要 | Sea surface temperature (SST) variability in the tropical Atlantic Ocean strongly impacts the climate on the surrounding continents. On interannual time scales, highest SST variability occurs in the eastern equatorial region and off the coast of southwestern Africa. The pattern of SST variability resembles the Pacific El Niño, but features notable differences, and has been discussed in the context of various climate modes, that is, reoccurring patterns resulting from particular interactions in the climate system. Here, we attempt to reconcile those different definitions, concluding that almost all of them are essentially describing the same mode that we refer to as the “Atlantic Niño.” We give an overview of the mechanisms that have been proposed to underlie this mode, and we discuss its interaction with other climate modes within and outside the tropical Atlantic. The impact of Atlantic Niño-related SST variability on rainfall, in particular over the Gulf of Guinea and north eastern South America is also described. An important aspect we highlight is that the Atlantic Niño and its teleconnections are not stationary, but subject to multidecadal modulations. Simulating the Atlantic Niño proves a challenge for state-of-the-art climate models, and this may be partly due to the large mean state biases in the region. Potential reasons for these model biases and implications for seasonal prediction are discussed. This article is categorized under: Climate Models and Modeling > Knowledge Generation with Models. © 2018 Wiley Periodicals, Inc. |
英文关键词 | Atlantic Niño; climate models; climate variability; tropical Atlantic |
语种 | 英语 |
scopus关键词 | Climatology; Oceanography; Surface waters; Tropics; Climate variability; Equatorial regions; Interannual time scale; Knowledge generations; Sea surface temperature (SST); Seasonal prediction; State of the art; Tropical atlantic; Climate models; annual variation; climate modeling; climate prediction; climate variation; computer simulation; sea surface temperature; teleconnection; timescale; Atlantic Ocean; Atlantic Ocean (Equatorial); Atlantic Ocean (Tropical); Gulf of Guinea; South America |
来源期刊 | Wiley Interdisciplinary Reviews: Climate Change
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/129948 |
作者单位 | GEOMAR Helmholtz Centre for Ocean Research, Kiel, Germany; Christian-Albrechts-Universität zu Kiel, Kiel, Germany; Departamento de Física de la Tierra y Astrofísica, Universidad Complutense de Madrid, Madrid, Spain; Instituto de Geociencias (IGEO), CSIC-UCM, Madrid, Spain; Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan; CECI/CERFACS, Toulouse, France; Department of Meteorology, University of Reading, Reading, United Kingdom; Geophysical Institute, University of Bergen, Bergen, Norway; Bjerknes Centre for Climate Research, Bergen, Norway |
推荐引用方式 GB/T 7714 | Lübbecke J.F.,Rodríguez-Fonseca B.,Richter I.,等. Equatorial Atlantic variability—Modes, mechanisms, and global teleconnections[J],2018,9(4). |
APA | Lübbecke J.F..,Rodríguez-Fonseca B..,Richter I..,Martín-Rey M..,Losada T..,...&Keenlyside N.S..(2018).Equatorial Atlantic variability—Modes, mechanisms, and global teleconnections.Wiley Interdisciplinary Reviews: Climate Change,9(4). |
MLA | Lübbecke J.F.,et al."Equatorial Atlantic variability—Modes, mechanisms, and global teleconnections".Wiley Interdisciplinary Reviews: Climate Change 9.4(2018). |
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