Institutional Repository of Key Laboratory of Ocean Circulation and Wave Studies, Institute of Oceanology, Chinese Academy of Sciences
| Representing surface wind stress response to mesoscale SST perturbations in western coast of South America using Tikhonov regularization method | |
Cui Chaoran1,2,3 ; Zhang Rong-Hua1,2,3,4; Wang Hongna1,2,4; Wei Yanzhou5
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| 2020-05-01 | |
| 发表期刊 | JOURNAL OF OCEANOLOGY AND LIMNOLOGY
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| ISSN | 2096-5508 |
| 卷号 | 38期号:3页码:679-694 |
| 通讯作者 | Zhang Rong-Hua(rzhang@qdio.ac.cn) |
| 摘要 | Interaction between mesoscale perturbations of sea surface temperature (SSTmeso) and wind stress (WSmeso) has great influences on the ocean upwelling system and turbulent mixing in the atmospheric boundary layer. Using daily Quik-SCAT wind speed data and AMSR-E SST data, SSTmeso and WSmeso fields in the western coast of South America are extracted by using a locally weighted regression method (LOESS). The spatial patterns of SSTmeso and WSmeso indicate strong mesoscale SST-wind stress coupling in the region. The coupling coefficient between SSTmeso and WSmeso is about 0.009 5 N/(m(2.)degrees C) in winter and 0.008 2 N/(m(2.)degrees C) in summer. Based on mesoscale coupling relationships, the mesoscale perturbations of wind stress divergence (Div(WSmeso)) and curl (Curl (WSmeso)) can be obtained from the SST gradient perturbations, which can be further used to derive wind stress vector perturbations using the Tikhonov regularization method. The computational examples are presented in the western coast of South America and the patterns of the reconstructed WSmeso are highly consistent with SSTmeso, but the amplitude can be underestimated significantly. By matching the spatially averaged maximum standard deviations of reconstructed WSmeso magnitude and observations, a reasonable magnitude of WSmeso can be obtained when a rescaling factor of 2.2 is used. As current ocean models forced by prescribed wind cannot adequately capture the mesoscale wind stress response, the empirical wind stress perturbation model developed in this study can be used to take into account the feedback effects of the mesoscale wind stress-SST coupling in ocean modeling. Further applications are discussed for taking into account the feedback effects of the mesoscale coupling in large-scale climate models and the uncoupled ocean models. |
| 关键词 | mesoscale air-sea coupling Tikhonov's regularization method western coast of South America |
| DOI | 10.1007/s00343-019-9042-8 |
| 收录类别 | SCI |
| 语种 | 英语 |
| WOS研究方向 | Marine & Freshwater Biology ; Oceanography |
| WOS类目 | Limnology ; Oceanography |
| WOS记录号 | WOS:000536606000008 |
| 出版者 | SCIENCE PRESS |
| 引用统计 | |
| 文献类型 | 期刊论文 |
| 条目标识符 | http://ir.qdio.ac.cn/handle/337002/167570 |
| 专题 | 海洋环流与波动重点实验室 |
| 通讯作者 | Zhang Rong-Hua |
| 作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao 266071, Peoples R China 2.Chinese Acad Sci, Ctr Ocean Megasci, Qingdao 266071, Peoples R China 3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 4.Qingdao Natl Lab Marine Sci & Technol, Qingdao 266000, Peoples R China 5.Minist Nat Resources, State Key Lab Satellite Ocean Environm Dynam, Inst Oceanog 2, Hangzhou 310012, Peoples R China |
| 第一作者单位 | 海洋环流与波动重点实验室; 中国科学院海洋大科学研究中心 |
| 通讯作者单位 | 海洋环流与波动重点实验室; 中国科学院海洋大科学研究中心 |
| 推荐引用方式 GB/T 7714 | Cui Chaoran,Zhang Rong-Hua,Wang Hongna,et al. Representing surface wind stress response to mesoscale SST perturbations in western coast of South America using Tikhonov regularization method[J]. JOURNAL OF OCEANOLOGY AND LIMNOLOGY,2020,38(3):679-694. |
| APA | Cui Chaoran,Zhang Rong-Hua,Wang Hongna,&Wei Yanzhou.(2020).Representing surface wind stress response to mesoscale SST perturbations in western coast of South America using Tikhonov regularization method.JOURNAL OF OCEANOLOGY AND LIMNOLOGY,38(3),679-694. |
| MLA | Cui Chaoran,et al."Representing surface wind stress response to mesoscale SST perturbations in western coast of South America using Tikhonov regularization method".JOURNAL OF OCEANOLOGY AND LIMNOLOGY 38.3(2020):679-694. |
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