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DOI | 10.1007/s00382-020-05268-5 |
Contribution of oceanic wave propagation from the tropical Pacific to asymmetry of the Ningaloo Niño/Niña | |
Kusunoki H.; Kido S.; Tozuka T. | |
发表日期 | 2020 |
ISSN | 0930-7575 |
起始页码 | 4865 |
结束页码 | 4875 |
卷号 | 54 |
英文摘要 | Ningaloo Niño/Niña is the dominant mode of interannual variability of sea surface temperature (SST) in the southeastern Indian Ocean. According to previous studies, both local air-sea interaction and remote forcing contribute to generation and amplification of the Ningaloo Niño/Niña. The latter forcing includes the atmospheric teleconnection and oceanic wave propagation through the Indonesian archipelago, mainly associated with the El Niño/Southern Oscillation (ENSO). One of the most important characteristics of the Ningaloo Niño/Niña is their asymmetry; the Ningaloo Niño is stronger than the Ningaloo Niña. Using a regional ocean modeling system (ROMS), the impact of oceanic wave propagation on the amplitude and asymmetry of SST anomalies associated with the Ningaloo Niño/Niña is investigated. For these purposes, a sensitivity experiment in which oceanic lateral boundary conditions are replaced by the monthly climatology is conducted. It is shown that the oceanic teleconnection transmitted from the western tropical Pacific can explain about 30% of the observed amplitude asymmetry in SST anomalies. Results from composite and heat budget analyses suggest that coastal downwelling (upwelling) Kelvin waves from the western tropical Pacific associated with La Niña (El Niño) that often co-occurs with the Ningaloo Niño (Niña) are stronger (weaker) and contribute to the asymmetry. © 2020, Springer-Verlag GmbH Germany, part of Springer Nature. |
英文关键词 | Coastal Kelvin wave; Ningaloo Niño/Niña; Regional ocean model; Western Australian coast |
语种 | 英语 |
scopus关键词 | air-sea interaction; annual variation; asymmetry; El Nino-Southern Oscillation; heat budget; Kelvin wave; La Nina; ocean wave; sea surface temperature; teleconnection; temperature anomaly; wave propagation; Indian Ocean; Indian Ocean (Southeast); Pacific Ocean; Pacific Ocean (Tropical) |
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/145459 |
作者单位 | Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo, 7-3-1 Hongo, Bunkyo-ku, Tokyo, 113-0033, Japan; Application Laboratory (APL), Research Institute for Value‐Added‐Information Generation (VAiG), Japan Agency for Marine‐Earth Science and Technology (JAMSTEC), Yokohama, Japan |
推荐引用方式 GB/T 7714 | Kusunoki H.,Kido S.,Tozuka T.. Contribution of oceanic wave propagation from the tropical Pacific to asymmetry of the Ningaloo Niño/Niña[J],2020,54. |
APA | Kusunoki H.,Kido S.,&Tozuka T..(2020).Contribution of oceanic wave propagation from the tropical Pacific to asymmetry of the Ningaloo Niño/Niña.Climate Dynamics,54. |
MLA | Kusunoki H.,et al."Contribution of oceanic wave propagation from the tropical Pacific to asymmetry of the Ningaloo Niño/Niña".Climate Dynamics 54(2020). |
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