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Sea surface cooling in the Northern South China Sea observed using Chinese sea-wing underwater glider measurements
文献类型：期刊论文
| 作者 | Qiu, Chunhua1,2; Mao, Huabin3; Yu, Jiancheng5; Xie, Qiang4 ; Wu, Jiaxue1,2; Lian, Shumin3; Liu, Qinyan3
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| 刊名 | DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS
 |
| 出版日期 | 2015-11-01 |
| 卷号 | 105页码:111-118 |
| 关键词 | Sea Surface Cooling Sea-wing Underwater Glider Mixed Layer Depth Heat Budget |
| DOI | 10.1016/j.dsr.2015.08.009 |
| 文献子类 | Article |
| 英文摘要 | Based on 26 days of Chinese Sea-wing underwater glider measurements and satellite microwave data, we documented cooling of the upper mixed layer of the ocean in response to changes in the wind in the Northern South China Sea (NSCS) from September 19, 2014, to October 15, 2014. The Sea-wing underwater glider measured 177 profiles of temperature, salinity, and pressure within a 55 km x 55 km area, and reached a depth of 1000 m at a temporal resolution of 4 h. The study area experienced two cooling events, Cooling 1 and Cooling 11, according to their timing. During Cooling I, water temperature at 1-m depth (T-1) decreased by similar to 1.0 degrees C, and the corresponding satellite-derived surface winds increased locally by 4.2 m/s. During Cooling II, T-1 decreased sharply by 1.7 degrees C within a period of 4 days; sea surface winds increased by 7 m/s and covered the entire NSCS. The corresponding mixed layer depth (MLD) deepened sharply from 30 m to 60 m during Cooling II, and remained steady during Cooling I. We estimated temperature tendencies using a ML model. High resolution Sea-wing underwater glider measurements provided an estimation of MLD migration, allowing us to obtain the temporal entrainment rate of cool sub-thermocline water. Quantitative analysis confirmed that the entrainment rate and latent heat flux were the two major components that regulated cooling of the ML and that the Ekman advection and sensible heat flux were small. (C) 2015 Elsevier Ltd. All rights reserved. |
| WOS关键词 | UPPER OCEAN RESPONSE ; MIXED-LAYER DEPTH ; INDIAN-OCEAN ; CIRCULATION |
| 语种 | 英语 |
| WOS记录号 | WOS:000364349300009 |
| 源URL | [http://124.16.218.2:8080/handle/183446/890]  |
| 专题 | 深海科学研究部_海洋环流观测与数值模拟研究室 |
| 作者单位 | 1.Sun Yat Sen Univ, Sch Marine Sci, Ctr Coastal Ocean Sci & Technol, Guangzhou 510275, Guangdong, Peoples R China 2.Sun Yat Sen Univ, Sch Marine Sci, Guangdong Prov Key Lab Marine Resources & Coastal, Guangzhou 510275, Guangdong, Peoples R China 3.Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, Beijing 510301, Peoples R China 4.Chinese Acad Sci, Sanya Inst Deep Sea Sci Engn, Beijing 572000, Peoples R China 5.Chinese Acad Sci, Shenyang Inst Automat, State Key Lab Robot, Shenyang 110016, Peoples R China |
| 推荐引用方式 GB/T 7714 | Qiu, Chunhua,Mao, Huabin,Yu, Jiancheng,et al. Sea surface cooling in the Northern South China Sea observed using Chinese sea-wing underwater glider measurements[J]. DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS,2015,105:111-118. |
| APA | Qiu, Chunhua.,Mao, Huabin.,Yu, Jiancheng.,Xie, Qiang.,Wu, Jiaxue.,...&Liu, Qinyan.(2015).Sea surface cooling in the Northern South China Sea observed using Chinese sea-wing underwater glider measurements.DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS,105,111-118. |
| MLA | Qiu, Chunhua,et al."Sea surface cooling in the Northern South China Sea observed using Chinese sea-wing underwater glider measurements".DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS 105(2015):111-118. |
入库方式： OAI收割
来源：深海科学与工程研究所
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