Interannual oscillation of meridional sea level wind and its impact on sea surface temperature in the South China Sea

Zhou Fa-xiu; Yu Shen-yu; Liu Qi

doi:10.1007/BF02848211

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Interannual oscillation of meridional sea level wind and its impact on sea surface temperature in the South China Sea

OriginalPaper | Updated：2023-05-16

- Interannual oscillation of meridional sea level wind and its impact on sea surface temperature in the South China Sea
- Interannual oscillation of meridional sea level wind and its impact on sea surface temperature in the South China Sea
- 海洋湖沼学报（英文） 1998年16卷第1期页码：9-16
- Affiliations：
  
  Dept. of Marine Meteorology
- Author bio：
- Funds：
  
  Project 49676276 supported by NSFC and also supported by FSEC.
- DOI：10.1007/BF02848211
  中图分类号：
- 纸质出版：1998
- Accepted：
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Interannual oscillation of meridional sea level wind and its impact on sea surface temperature in the South China Sea[J]. 海洋湖沼学报（英文）, 1998,16(1):9-16.

Fa-xiu, Z., Shen-yu, Y. & Qi, L. Interannual oscillation of meridional sea level wind and its impact on sea surface temperature in the South China Sea., Chin. J. Ocean. Limnol. 16, 9–16 (1998). https://doi.org/10.1007/BF02848211
Interannual oscillation of meridional sea level wind and its impact on sea surface temperature in the South China Sea[J]. 海洋湖沼学报（英文）, 1998,16(1):9-16. DOI： 10.1007/BF02848211.

Fa-xiu, Z., Shen-yu, Y. & Qi, L. Interannual oscillation of meridional sea level wind and its impact on sea surface temperature in the South China Sea., Chin. J. Ocean. Limnol. 16, 9–16 (1998). https://doi.org/10.1007/BF02848211 DOI：

摘要

Abstract

Analysis of COADS data (1958–1987) showed that there is obviously interannual SST oscillation including QBO (Quasi-biennial oscillation) and quasi-3.5 year oscilation

etc.

of the SCS (South China Sea)

which is the response of the upper mixed layer of the sea to the impact of the East Asian Monsoon anomaly. Most SST anomalies appear in the central basin of the SCS. The phase-locked phenomena linking the SST annual cycle and interannual oscillation is an important characteristic of the SCS climate. There is not only SST response to atmospheric impact

but also feedback to the air. The authors put forward a scheme of regional air-sea interaction in winter time in the SCS.

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Keywords

references

Chen, L. X., Zhu, Q. G., 1991. The East Asian monsoons. Met. Press, Beijing, 362p. (in Chinese)

Ding, Y. H., 1990. A statistical study of winter monsoons in East Asia.Tropic Met. 6: 119–127. (in Chinese)

Fu, G., Zhou, F. X., 1994. The dynamic mechanism of the low frequency oscillation of SST in The South China Sea.Jour. of Ocean University of Qingdao 24(4): 456–462. (in Chinese with English abstract)

Yu, S. Y., Zhou, F. X., 1994. The basic features of the low frequency oscillations of SST in the South China Sea.Oceanol etLimnol.25(5): 546–551. (in Chinese with English abstract)

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