Sea surface temperature anomalies in the South China Sea during mature phase of ENSO

Fuwen Qiu; Aijun Pan; Shanwu Zhang; Jing Cha; Haowei Sun

doi:10.1007/s00343-016-4290-3

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Sea surface temperature anomalies in the South China Sea during mature phase of ENSO

OriginalPaper | Updated：2023-05-16

- Sea surface temperature anomalies in the South China Sea during mature phase of ENSO
- Sea surface temperature anomalies in the South China Sea during mature phase of ENSO
- 海洋湖沼学报（英文） 2016年34卷第3期页码：577-584
- Affiliations：
  
  Third Institute of Oceanography State Oceanic Administration
- Author bio：
- Funds：
  
  Supported by the National Natural Science Foundation of China (No. 41306026), the Scientific Research Foundation of the Third Institute of Oceanography, SOA (No. 2013009), the National Basic Research Program of China (973 Program) (No. 2011CB403504), and the National Special Research Fund for Non-Profit Marine Sector (No. 201005005-2)
- DOI：10.1007/s00343-016-4290-3
  中图分类号：
- 网络首发：2015-10-30，
  
  纸质出版：2016
- Accepted：
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Sea surface temperature anomalies in the South China Sea during mature phase of ENSO[J]. 海洋湖沼学报（英文）, 2016,34(3):577-584.

Qiu, F., Pan, A., Zhang, S. et al. Sea surface temperature anomalies in the South China Sea during mature phase of ENSO., Chin. J. Ocean. Limnol. 34, 577–584 (2016). https://doi.org/10.1007/s00343-016-4290-3
Sea surface temperature anomalies in the South China Sea during mature phase of ENSO[J]. 海洋湖沼学报（英文）, 2016,34(3):577-584. DOI： 10.1007/s00343-016-4290-3.

Qiu, F., Pan, A., Zhang, S. et al. Sea surface temperature anomalies in the South China Sea during mature phase of ENSO., Chin. J. Ocean. Limnol. 34, 577–584 (2016). https://doi.org/10.1007/s00343-016-4290-3 DOI：

摘要

Abstract

Based on the 18-year (1993–2010) National Centers for Environmental Prediction optimum interpolation sea surface temperature (SST) and simple ocean data assimilation datasets

this study investigated the patterns of the SST anomalies (SSTAs) that occurred in the South China Sea (SCS) during the mature phase of the El Niño/Southern Oscillation. The most dominant characteristic was that of the outof-phase variation between southwestern and northeastern parts of the SCS

which was influenced primarily by the net surface heat flux and by horizontal thermal advection. The negative SSTA in the northeastern SCS was caused mainly by the loss of heat to the atmosphere and because of the cold-water advection from the western Pacific through the Luzon Strait during El Niño episodes. Conversely

it was found that the anomalous large-scale atmospheric circulation and weakened western boundary current during El Niño episodes led to the development of the positive SSTA in the southwestern SCS.

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references

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