Trends of sea surface temperature and sea surface temperature fronts in the South China Sea during 2003–2017
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  • 英文篇名:Trends of sea surface temperature and sea surface temperature fronts in the South China Sea during 2003–2017
  • 作者:Yi ; Yu ; Hao-Ran ; Zhang ; Jiangbo ; Jin ; Yuntao ; Wang
  • 英文作者:Yi Yu;Hao-Ran Zhang;Jiangbo Jin;Yuntao Wang;State Key Laboratory of Satellite Ocean Environment Dynamics,Second Institute of Oceanography,Ministry of Natural Resources;College of Oceanography,Hohai University;International Center for Climate and Environment Sciences,Institute of Atmospheric Physics,Chinese Academy of Sciences;State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics,Institute of Atmospheric Physics,Chinese Academy of Sciences;
  • 英文关键词:South China Sea;;sea surface temperature;;sea surface temperature fronts;;warming trend;;wind stress
  • 中文刊名:SEAE
  • 英文刊名:海洋学报(英文版)
  • 机构:State Key Laboratory of Satellite Ocean Environment Dynamics,Second Institute of Oceanography,Ministry of Natural Resources;College of Oceanography,Hohai University;International Center for Climate and Environment Sciences,Institute of Atmospheric Physics,Chinese Academy of Sciences;State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics,Institute of Atmospheric Physics,Chinese Academy of Sciences;
  • 出版日期:2019-04-15
  • 出版单位:Acta Oceanologica Sinica
  • 年:2019
  • 期:v.38
  • 基金:The National Key Research and Development Program of China under contract No.2016YFC1401601;; the Scientific Research Fund of the Second Institute of Oceanography,MNR under contract No.JB1806;; the National Natural Science Foundation of China under contract Nos 41806026,41806041,41706036 and 41730536;; the Project of State Key Laboratory of Satellite Ocean Environment Dynamics,Second Institute of Oceanography,MNR under contract No.SOEDZZ1902
  • 语种:英文;
  • 页:SEAE201904012
  • 页数:10
  • CN:04
  • ISSN:11-2056/P
  • 分类号:110-119
摘要
The trends of the sea surface temperature(SST) and SST fronts in the South China Sea(SCS) are analyzed during2003–2017 using high-resolution satellite data. The linear trend of the basin averaged SST is 0.31°C per decade,with the strongest warming identified in southeastern Vietnam. Although the rate of warming is comparable in summer and winter for the entire basin, the corresponding spatial patterns of the linear trend are substantially different between them. The SST trend to the west of the Luzon Strait is characterized by rapid warming in summer, exceeding approximately 0.6°C per decade, but the trend is insignificant in winter. The strongest warming trend occurs in the southeast of Vietnam in winter, with much less pronounced warming in summer. A positive trend of SST fronts is identified for the coast of China and is associated with increasing wind stress. The increasing trend of SST fronts is also found in the east of Vietnam. Large-scale circulation, such as El Ni?o, can influence the trends of the SST and SST fronts. A significant correlation is found between the SST anomaly and Ni?o3.4 index, and the ENSO signal leads by eight months. The basin averaged SST linear trends increase after the El Ni?o event(2009–2010), which is, at least, due to the rapid warming rate causing by the enhanced northeasterly wind. Peaks of positive anomalous SST and negatively anomalous SST fronts are found to co-occur with the strong El Ni?o events.
        The trends of the sea surface temperature(SST) and SST fronts in the South China Sea(SCS) are analyzed during2003–2017 using high-resolution satellite data. The linear trend of the basin averaged SST is 0.31°C per decade,with the strongest warming identified in southeastern Vietnam. Although the rate of warming is comparable in summer and winter for the entire basin, the corresponding spatial patterns of the linear trend are substantially different between them. The SST trend to the west of the Luzon Strait is characterized by rapid warming in summer, exceeding approximately 0.6°C per decade, but the trend is insignificant in winter. The strongest warming trend occurs in the southeast of Vietnam in winter, with much less pronounced warming in summer. A positive trend of SST fronts is identified for the coast of China and is associated with increasing wind stress. The increasing trend of SST fronts is also found in the east of Vietnam. Large-scale circulation, such as El Ni?o, can influence the trends of the SST and SST fronts. A significant correlation is found between the SST anomaly and Ni?o3.4 index, and the ENSO signal leads by eight months. The basin averaged SST linear trends increase after the El Ni?o event(2009–2010), which is, at least, due to the rapid warming rate causing by the enhanced northeasterly wind. Peaks of positive anomalous SST and negatively anomalous SST fronts are found to co-occur with the strong El Ni?o events.
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