中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Mixed Layer Heat Variations in the South China Sea Observed by Argo Float and Reanalysis Data during 2012-2015

文献类型:期刊论文

作者Liang, Zhanlin4; Xing, Tao1,4,5; Wang, Yinxia3,6; Zeng, Lili; liangzl@scsio.ac.cn; xingtao@gmgs.cn; yinxiawang1227@gmail.com; zenglili@scsio.ac.cn
刊名SUSTAINABILITY
出版日期2019
卷号11期号:19页码:5429
关键词South China Sea Argo float mixed layer heat variation heat advection entrainment barrier layer residual
DOI10.3390/su11195429
英文摘要The atmospheric and oceanic causes of mixed layer heat variations in the South China Sea (SCS) are examined using data from six long-lived Array for Real-time Geostrophic Oceanography (Argo) floats. The mixed layer heat budget along each float trajectory is evaluated based on direct measurements, satellite and reanalysis datasets. Our results suggest that the mixed layer heat balance in the SCS has distinct spatial and seasonal variations. The amplitude of all terms in the mixed layer heat budget equation is significantly larger in the northern SCS than in the southern SCS, especially in winter. In the northern SCS, the mixed layer heat budget is controlled by the local surface heat flux and horizontal advection terms in winter, and the net heat flux term in summer. In the western and southeastern SCS, the mixed layer heat budget is dominated by the net surface heat flux in both winter and summer. Further analysis shows that in the SCS, surface shortwave radiation and geostrophic heat advection are major contributors to net heat flux and horizontal advection, respectively. Unlike the net heat flux and horizontal advection, the vertical entrainment is a sink term in general. The rate of mixed layer deepening is the most important factor in the entrainment rate, and a barrier layer may decrease the temperature difference between the bottom of the mixed layer and the water beneath. Residual analysis suggests that the residual term in the equation is due to the inexact calculation of heat geostrophic advection, other missing terms, and unresolved physical ocean dynamic processes.
资助机构National Natural Science Foundation of ChinaNational Natural Science Foundation of China (NSFC) [41606030, 41776025, 41776026, 41876018, 41806035, 41576012, 41876017]; Open Foundation of Key Laboratory of Technology for Safeguarding of Maritime Rights and Interests and Application, SOA [SCS1616] ; National Natural Science Foundation of ChinaNational Natural Science Foundation of China (NSFC) [41606030, 41776025, 41776026, 41876018, 41806035, 41576012, 41876017]; Open Foundation of Key Laboratory of Technology for Safeguarding of Maritime Rights and Interests and Application, SOA [SCS1616]
源URL[http://ir.scsio.ac.cn/handle/344004/18216]  
专题南海海洋研究所_热带海洋环境国家重点实验室(LTO)
作者单位1.Chinese Acad Sci, South China Sea Inst Oceanol, Key Lab Marginal Sea Geol, Guangzhou 510301, Guangdong, Peoples R China
2.SOA, Key Lab Technol Safeguarding Maritime Rights & In, Guangzhou 510301, Guangdong, Peoples R China
3.State Ocean Adm, South China Sea Inst Planning & Environm Res, Guangzhou 510301, Guangdong, Peoples R China
4.Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog LTO, Guangzhou 510301, Guangdong, Peoples R China
5.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
6.Guangzhou Marine Geol Survey, MLR Key Lab Marine Mineral Resources, Guangzhou 510075, Guangdong, Peoples R China
推荐引用方式
GB/T 7714
Liang, Zhanlin,Xing, Tao,Wang, Yinxia,et al. Mixed Layer Heat Variations in the South China Sea Observed by Argo Float and Reanalysis Data during 2012-2015[J]. SUSTAINABILITY,2019,11(19):5429.
APA Liang, Zhanlin.,Xing, Tao.,Wang, Yinxia.,Zeng, Lili.,liangzl@scsio.ac.cn.,...&zenglili@scsio.ac.cn.(2019).Mixed Layer Heat Variations in the South China Sea Observed by Argo Float and Reanalysis Data during 2012-2015.SUSTAINABILITY,11(19),5429.
MLA Liang, Zhanlin,et al."Mixed Layer Heat Variations in the South China Sea Observed by Argo Float and Reanalysis Data during 2012-2015".SUSTAINABILITY 11.19(2019):5429.

入库方式: OAI收割

来源:南海海洋研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。