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DOI | 10.1007/s00382-020-05391-3 |
Upscale feedback of high-frequency winds on seasonal SST change over the tropical western North Pacific during boreal summer | |
Wang Y.; Wu R.; Jiao Y. | |
发表日期 | 2020 |
ISSN | 0930-7575 |
起始页码 | 2439 |
结束页码 | 2451 |
卷号 | 55 |
英文摘要 | Present study compares the contribution of low-frequency (> 90-day) and high-frequency (< 90-day) variation-related latent heat flux (LHF) to seasonal sea surface temperature (SST) change during boreal summer. It is revealed that both low- and high-frequency LHFs have prominent but opposite contributions to seasonal SST change in the tropical western North Pacific (WNP) during boreal summer. The feedback of high-frequency LHF on the seasonal SST change in the WNP is strong during El Niño events but weak during La Niña events. The difference in the feedback of high-frequency LHF is due to two factors. One is the background surface wind and the other is the intensity of high-frequency wind fluctuations. The high-frequency LHF displays a large non-linear dependence on surface wind under the weak background surface wind during El Niño developing summers, which leads to an accumulation of high-frequency daily LHF in summer mean. The high-frequency wind variability is large over the WNP during El Niño developing summers, which further enhances the accumulation of high-frequency daily LHF. The strong background surface wind and relatively weak high-frequency wind variability during La Niña developing summers are unfavorable for the accumulation of high-frequency daily LHF. This leads to a small summer mean of high-frequency LHF so that the upscale feedback of high-frequency wind variations on seasonal SST change is weak in the WNP during La Niña developing summers. © 2020, Springer-Verlag GmbH Germany, part of Springer Nature. |
英文关键词 | El Niño and La Niña; High-frequency wind variations; Seasonal SST change; The western North Pacific; Upscale feedback |
语种 | 英语 |
scopus关键词 | climate feedback; El Nino; La Nina; latent heat flux; sea surface temperature; seasonal variation; summer; surface wind; Pacific Ocean; Pacific Ocean (North) |
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/145305 |
作者单位 | Center for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China; College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, China; School of Earth Sciences, Zhejiang University, Hangzhou, China; Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, China; Guangzhou Meteorological Observatory, Guangzhou, China |
推荐引用方式 GB/T 7714 | Wang Y.,Wu R.,Jiao Y.. Upscale feedback of high-frequency winds on seasonal SST change over the tropical western North Pacific during boreal summer[J],2020,55. |
APA | Wang Y.,Wu R.,&Jiao Y..(2020).Upscale feedback of high-frequency winds on seasonal SST change over the tropical western North Pacific during boreal summer.Climate Dynamics,55. |
MLA | Wang Y.,et al."Upscale feedback of high-frequency winds on seasonal SST change over the tropical western North Pacific during boreal summer".Climate Dynamics 55(2020). |
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