中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Spatial-Temporal Variations and Mechanisms of the Upper Ocean Heat Content in the South China Sea

文献类型:期刊论文

作者Liu, Hongwei1,2,5; Zhang, Qilong1,2,5; Pang, Chongguang1,2,5; Cai, Rongshuo3; Qi, Qinghua3; Zheng, Dongmei4
刊名PURE AND APPLIED GEOPHYSICS
出版日期2019-04-01
卷号176期号:4页码:1847-1861
关键词The South China Sea Heat content spatial and temporal variation regime shift
ISSN号0033-4553
DOI10.1007/s00024-018-2051-2
通讯作者Liu, Hongwei(liuhongwei@qdio.ac.cn)
英文摘要The variability of the upper ocean heat content (OHC) of the South China Sea (SCS) has a significant regional climate impact on the surrounding East and Southeast Asian countries. In this paper, the spatial-temporal variations of the upper OHC in the SCS and their relations to El Nino-Southern Oscillation (ENSO) are analyzed using empirical orthogonal functions and correlation analysis. The mechanisms for the interannual OHC variability associated with ENSO and regime shift in 1998 are further examined using composite and correlation analysis methods. The results show that the OHC anomaly field is mainly composed of two leading modes, i.e., an in-phase oscillation mode and a zonal anti-phase oscillation mode. The in-phase oscillation mode exhibits strong interannual variability with periods of 2-5years, which is well related to ENSO at a lead of 6months, and experienced a regime shift in 1998. The anti-phase oscillation mode shows only a strong interannual variability with periods of 2-4years well related to ENSO at a lag of 4months. The composite analysis reveals that horizontal thermal advection mainly controlled by wind forcing plays a primary role in modulating the interannual OHC variability associated with ENSO, while net surface heat flux is the secondary source. And the OHC regime shift in 1998 primarily results from both the strong cold advection during the extremely strong El Nino in 1997 and the subsequent warm advection during the strong La Nina in 1998.
资助项目National Natural Science Foundation of China[41406012] ; National Natural Science Foundation of China[41576060] ; National Key R&D Program of China[2016YFC0301203] ; Open Fund of Key Laboratory of Global Change and Marine-Atmospheric Chemistry, State Oceanic Administration, China[GCMAC1501] ; Open Fund of State Key Laboratory of Satellite Ocean Environment Dynamics (Second Institute of Oceanography)[SOED1613] ; NSFC-Shandong Joint Fund for Marine Science Research Centers[U1406401]
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000463789200029
出版者SPRINGER BASEL AG
源URL[http://ir.qdio.ac.cn/handle/337002/161194]  
专题海洋研究所_海洋环流与波动重点实验室
通讯作者Liu, Hongwei
作者单位1.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, 7 Nanhai Rd, Qingdao 266071, Peoples R China
2.Qingdao Natl Lab Marine Sci & Technol, 7 Nanhai Rd, Qingdao 266071, Peoples R China
3.State Ocean Adm, Inst Oceanog 3, Key Lab Global Change & Marine Atmospher Chem, Xiamen 361005, Peoples R China
4.Marine Environm Forecasting & Disaster Preventing, Shenyang 110001, Liaoning, Peoples R China
5.Chinese Acad Sci, Ctr Ocean Mega Sci, 7 Nanhai Rd, Qingdao 266071, Shandong, Peoples R China
推荐引用方式
GB/T 7714
Liu, Hongwei,Zhang, Qilong,Pang, Chongguang,et al. Spatial-Temporal Variations and Mechanisms of the Upper Ocean Heat Content in the South China Sea[J]. PURE AND APPLIED GEOPHYSICS,2019,176(4):1847-1861.
APA Liu, Hongwei,Zhang, Qilong,Pang, Chongguang,Cai, Rongshuo,Qi, Qinghua,&Zheng, Dongmei.(2019).Spatial-Temporal Variations and Mechanisms of the Upper Ocean Heat Content in the South China Sea.PURE AND APPLIED GEOPHYSICS,176(4),1847-1861.
MLA Liu, Hongwei,et al."Spatial-Temporal Variations and Mechanisms of the Upper Ocean Heat Content in the South China Sea".PURE AND APPLIED GEOPHYSICS 176.4(2019):1847-1861.

入库方式: OAI收割

来源:海洋研究所

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