Institutional Repository of Key Laboratory of Ocean Circulation and Wave Studies, Institute of Oceanology, Chinese Academy of Sciences
Ocean dynamical processes associated with the tropical Pacific cold tongue mode | |
Li, Yang1,2; Li, Jianping2,3; Zhang, Wenjun4; Zhao, Xia5; Xie, Fei2,3; Zheng, Fei6 | |
2015-09-01 | |
发表期刊 | JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS |
卷号 | 120期号:9页码:6419-6435 |
文章类型 | Article |
摘要 | The cold tongue mode (CTM) is the second EOF mode of sea surface temperature anomaly (SSTA) variability over the tropical Pacific and represents the out- of- phase relationship in SSTA variability between the Pacific cold tongue region and elsewhere in the tropical Pacific. A positive CTM is characterized by cold SSTA in the Pacific cold tongue region and warm SSTA in the rest of the tropical Pacific, with conditions reversed for a negative CTM. The CTM is a coupled air- sea mode, and its long- term variability is most probably induced by ocean dynamical processes in response to global warming [ Zhang et al., 2010]. This study focuses on the specific ocean dynamical processes associated with the CTM and its possible relationship with global warming. A heat budget diagnosis of ocean temperature in the eastern equatorial Pacific shows that the net heat flux plays a damping role and the four ocean advection terms (2u0@ T =@ x, 2 v@ T0=@ y, 2 w@ T0=@ z, and 2w0@ T =@ z) contribute to the temperature change associated with the CTM. Among them, the vertical advection of the anomalous temperature by the mean upwelling (2 w@ T0=@ z) makes a dominant contribution to the long- term change in the CTM. The long- term change of the term 2 w@ T0=@ z is controlled mainly by the decreasing vertical gradient of the ocean temperature anomaly (@ T0=@ z). The other three advection terms make a minor contribution to the long- term change in the CTM. |
关键词 | Cold Tongue Mode Ocean Dynamical Processes Long-term Variability Global Warming Eastern Equatorial Pacific |
DOI | 10.1002/2015JC010814 |
收录类别 | SCI |
语种 | 英语 |
WOS记录号 | WOS:000363470300030 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://ir.qdio.ac.cn/handle/337002/73942 |
专题 | 海洋环流与波动重点实验室 海洋地质与环境重点实验室 |
作者单位 | 1.Lanzhou Univ, Coll Atmospher Sci, Lanzhou 730000, Peoples R China 2.Beijing Normal Univ, Coll Global Change & Earth Syst Sci, Beijing 100875, Peoples R China 3.Joint Ctr Global Change Studies, Beijing, Peoples R China 4.Nanjing Univ Informat Sci & Technol, Minist Educ, Key Lab Meteorol Disaster, Collaborat Innovat Ctr Forecast & Evaluat Meteorl, Nanjing, Jiangsu, Peoples R China 5.Chinese Acad Sci, Inst Oceanol, Lab Ocean Circulat & Waves, Qingdao, Peoples R China 6.Chinese Acad Sci, State Key Lab Numer Modeling Atmospher Sci & Geop, Inst Atmospher Phys, Beijing, Peoples R China |
推荐引用方式 GB/T 7714 | Li, Yang,Li, Jianping,Zhang, Wenjun,et al. Ocean dynamical processes associated with the tropical Pacific cold tongue mode[J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,2015,120(9):6419-6435. |
APA | Li, Yang,Li, Jianping,Zhang, Wenjun,Zhao, Xia,Xie, Fei,&Zheng, Fei.(2015).Ocean dynamical processes associated with the tropical Pacific cold tongue mode.JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,120(9),6419-6435. |
MLA | Li, Yang,et al."Ocean dynamical processes associated with the tropical Pacific cold tongue mode".JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS 120.9(2015):6419-6435. |
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文件名称/大小 | 文献类型 | 版本类型 | 开放类型 | 使用许可 | ||
Ocean dynamical proc(3048KB) | 期刊论文 | 出版稿 | 限制开放 | CC BY-NC-SA | 浏览 |
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