Sea surface cooling in the Northern South China Sea observed using Chinese sea-wing underwater glider measurements | |
Qiu CH(邱春华); Mao HB(毛华斌); Yu JC(俞建成); Xie, Qiang; Wu, Jiaxue; Lian SM(练树民); Liu, Qinyan | |
刊名 | Deep-Sea Research Part I: Oceanographic Research Papers |
2015 | |
卷号 | 105页码:111-118 |
关键词 | Sea Surface Cooling Sea-wing Underwater Glider Mixed Layer Depth Heat Budget |
ISSN号 | 0967-0637 |
产权排序 | 3 |
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 55km×55km area, and reached a depth of 1000m at a temporal resolution of ~4h. The study area experienced two cooling events, Cooling I and Cooling II, according to their timing. During Cooling I, water temperature at 1-m depth (T1) decreased by ~1.0°C, and the corresponding satellite-derived surface winds increased locally by 4.2m/s. During Cooling II, T1 decreased sharply by 1.7°C within a period of 4 days; sea surface winds increased by 7m/s and covered the entire NSCS. The corresponding mixed layer depth (MLD) deepened sharply from 30m to 60m 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. |
WOS关键词 | UPPER OCEAN RESPONSE ; MIXED-LAYER DEPTH ; INDIAN-OCEAN ; CIRCULATION |
WOS研究方向 | Oceanography |
语种 | 英语 |
WOS记录号 | WOS:000364349300009 |
资助机构 | National Natural Science Foundation of China(41406043, 41406002, and 61233013), National Basic Research Program of China(2013CB956502), and the Fundamental Research Funds for the Central Universities. |
内容类型 | 期刊论文 |
源URL | [http://ir.sia.cn/handle/173321/16976] |
专题 | 沈阳自动化研究所_水下机器人研究室 |
通讯作者 | Mao HB(毛华斌) |
作者单位 | 1.State key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, China 2.Sanya Institute of Deep-sea Science of Engineering, Chinese Academy of Sciences, China 3.Guangdong Provincial Key Laboratory of Marine Resources and Coastal Engineering, School of Marine Sciences, Sun Yat-sen University, China 4.The Center for Coastal Ocean Science and Technology, School of Marine Sciences, Sun Yat-sen University, China 5.State Key Laboratory of Robotics, Shenyang Institute of Automation, Chinese Academy of Sciences, China |
推荐引用方式 GB/T 7714 | Qiu CH,Mao HB,Yu JC,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 CH.,Mao HB.,Yu JC.,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 CH,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. |
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