The regional feature of the sea surface temperature anomalies in the Tropical West Pacific

Zhou Faxiu; Yu Shenyu

doi:10.1007/BF02850673

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The regional feature of the sea surface temperature anomalies in the Tropical West Pacific

OriginalPaper | Updated：2023-05-16

- The regional feature of the sea surface temperature anomalies in the Tropical West Pacific
- The regional feature of the sea surface temperature anomalies in the Tropical West Pacific
- 海洋湖沼学报（英文） 1991年9卷第2期页码：146-152
- Affiliations：
  
  Ocean University of Qingdao
- Author bio：
- Funds：
  
  This paper was published in Chinese in;Oceanologia et Limnologia Sinica;21;(2): 97–104, 1990.
- DOI：10.1007/BF02850673
  中图分类号：
- 纸质出版：1991
- Accepted：
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The regional feature of the sea surface temperature anomalies in the Tropical West Pacific[J]. 海洋湖沼学报（英文）, 1991,9(2):146-152.

Faxiu, Z., Shenyu, Y. The regional feature of the sea surface temperature anomalies in the Tropical West Pacific., Chin. J. Ocean. Limnol. 9, 146–152 (1991). https://doi.org/10.1007/BF02850673
The regional feature of the sea surface temperature anomalies in the Tropical West Pacific[J]. 海洋湖沼学报（英文）, 1991,9(2):146-152. DOI： 10.1007/BF02850673.

Faxiu, Z., Shenyu, Y. The regional feature of the sea surface temperature anomalies in the Tropical West Pacific., Chin. J. Ocean. Limnol. 9, 146–152 (1991). https://doi.org/10.1007/BF02850673 DOI：

摘要

Abstract

The complex empirical orthogonal function is employed to analyse the monthly sea surface temperature anomalies (SSTA) in the Tropical West Pacific (TWP) for the period from 1951 to 1986. The results show that the SSTA in the area appear in three patterns: a quasi-stationary mode

a latitudinally propagating mode and a longitudinally propagating mode. The three modes contribute almost equally to the total variance of SST. Digital filtering

time-lag correlation

etc.

are applied to analyse the quasi-period low frequency oscillations of the modes and their relations to the southern oscillation (SO) and the West Pacific Subtropical High (WPSH). The SSTA in the TWP is different from that in an ocean current area and plays a special role in the large scale air-sea interaction. Aside from being related to the SSTA in the Equatorial East Pacific

the SSTA in the TWP

on the one hand

respond to the oscillation of the global sea level pressure and influence the Subtropical High

and on the other hand receive feedback from the Subtropical High.

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Keywords

references

Barnett, T. P. 1983. Interaction of the monsoon and Pacific trade wind system at interannual time scales. Part 1: The equatorial zone.Mon. Wea. Rev. 111: 756–773.

Krishnamurti, T. N., 1987. Tropical Meteorology, Meteor. Pul. Beijing pp 12–15 (Chinese translation).

Krishnamurti, T. N., Chu Shaohang and W. Iglesias, 1986. On the sea level pressure of the southern oscillation.Arch. Met. Geoph. Biocl. Ser. A 34: 385–425.

Murakami, M. 1979. Large-scale aspects of deep convective activity over the GATE area,Mon. Wea. Rev. 107: 994–1013.

Wang Shaowu, Zhao Zongci, Cheng Zhenxue et al., 1980. Air sea interactions in winter.Acta Oceanologica Sinica 2(2): 27–29 (in Chinese).

Wang Shaowu and Zhou Zongci, 1984. The Base of Long-term Weather Prediction, Shanghai Science Press pp. 157–158 (in Chinese).

Yu Shenyu and Zhou Faxiu, 1988. The relationship between the low frequency oscillations of the sea surface temperature in the Kuroshio region and that in the Equatorial Eastern Pacific.Oceanologia et Limnologia Sinica 19 (5): 485–493 (in Chinese with English abstract).

Zhou Faxiu and Yu Shenyu, 1989. The low frequency oscillations of the sea surface temperature in the Equatorial Eastern Pacific and El Niño formation.Acta Oceanologica Sinica 8 (4): 59–71.

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