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DOI | 10.1175/JCLI-D-19-1020.1 |
Depth structure of ningaloo niño/niña events and associated drivers | |
Ryan S.; Ummenhofer C.C.; Gawarkiewicz G.; Wagner P.; Scheinert M.; Biastoch A.; Böning C.W. | |
发表日期 | 2021 |
ISSN | 08948755 |
起始页码 | 1767 |
结束页码 | 1788 |
卷号 | 34期号:5 |
英文摘要 | Marine heatwaves along the coast of Western Australia, referred to as Ningaloo Niño, have had dramatic impacts on the ecosystem in the recent decade. A number of local and remote forcing mechanisms have been put forward; however, little is known about the depth structure of such temperature extremes. Utilizing an eddy-active global ocean general circulation model, Ningaloo Niño and the corresponding cold Ningaloo Niña events are investigated between 1958 and 2016, with a focus on their depth structure. The relative roles of buoyancy and wind forcing are inferred from sensitivity experiments. Composites reveal a strong symmetry between cold and warm events in their vertical structure and associated large-scale spatial patterns. Temperature anomalies are largest at the surface, where buoyancy forcing is dominant, and extend down to 300-m depth (or deeper), with wind forcing being the main driver. Large-scale subsurface anomalies arise from a vertical modulation of the thermocline, extending from the western Pacific into the tropical eastern Indian Ocean. The strongest Ningaloo Niños in 2000 and 2011 are unprecedented compound events, where long-lasting high temperatures are accompanied by extreme freshening, which emerges in association with La Niñas, that is more common and persistent during the negative phase of the interdecadal Pacific oscillation. It is shown that Ningaloo Niños during La Niña phases have a distinctively deeper reach and are associated with a strengthening of the Leeuwin Current, while events during El Niño are limited to the surface layer temperatures, likely driven by local atmosphere-ocean feedbacks, without a clear imprint on salinity and velocity. © 2021 American Meteorological Society. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy (www.ametsoc.org/PUBSReuseLicenses). |
英文关键词 | Australia; Extreme events; General circulation models; Indian Ocean; Ocean; Ocean models |
语种 | 英语 |
scopus关键词 | Buoyancy; Composite structures; Lanthanum; Buoyancy forcing; Inter-decadal pacific oscillations; Surface layer temperature; Temperature anomaly; Temperature extremes; Vertical modulation; Vertical structures; Western Australia; Atmospheric temperature; air-sea interaction; atmospheric general circulation model; buoyancy; decadal variation; El Nino; extreme event; heat wave; La Nina; Pacific Decadal Oscillation; temperature anomaly; wind forcing; Australia; Indian Ocean; Western Australia |
来源期刊 | Journal of Climate
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/178712 |
作者单位 | Woods Hole Oceanographic Institution, Woods Hole, MA, United States; ARC Centre of Excellence for Climate Extremes, University of New South Wales, Sydney, NSW, Australia; GEOMAR, Helmholtz Centre for Ocean Research Kiel, Kiel, Germany |
推荐引用方式 GB/T 7714 | Ryan S.,Ummenhofer C.C.,Gawarkiewicz G.,et al. Depth structure of ningaloo niño/niña events and associated drivers[J],2021,34(5). |
APA | Ryan S..,Ummenhofer C.C..,Gawarkiewicz G..,Wagner P..,Scheinert M..,...&Böning C.W..(2021).Depth structure of ningaloo niño/niña events and associated drivers.Journal of Climate,34(5). |
MLA | Ryan S.,et al."Depth structure of ningaloo niño/niña events and associated drivers".Journal of Climate 34.5(2021). |
条目包含的文件 | 条目无相关文件。 |
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