-
Abstract:
The Singular Spectrum Analysis (SSA) method is used to conduct studies of periodicity of the SST and meridional winds in tropical Pacific Ocean. The results show that the air-sea system for the Pacific varies on quasi-4-year, quasi-2-year and interannual scales, with the quasi-4-year scale having the highest variability. Depending on the scale, the wind field has a varying degree of association with the SST anomalies. Difference is also found in the evolution of phase. In addition, the work discusses the difference in SSTA resulted from wind fields for quasi-4-year and quasi-2-year components.
-
References
[1]
|
BJERKNES J. A possible response of the atmospheric Hadley circulation to equatorial anomalies of oceantemperature [J]. Monthly Weather Review, 1966, 18: 820-829. |
[2]
|
BJERKNES J. Atmospheric teleconnections from the equatorial Pacific [J]. Monthly Weather Review, 1969,97:163-172.. |
[3]
|
BJERKNES J. Large-scale atmospheric response to the 1964~1965 Pacific equatorial warming [J]. Journalof Physics Oceanography, 1972, 2: 212-217. |
[4]
|
RASMUSSON E M, WANG X L, ROPELEWSKI C. The biennial component of ENSO variability [J]. J Mar.Sys., 1990, 1: 71-96. |
[5]
|
YASUNARI T. Role of Asian monsoon on the interannual variability of the global climate system [J]. JMeteor Soc Japan, 1992, 70: 177-189. |
[6]
|
HE Jin-hai et al. Seasonal variation of the air-sea relationship over equatorial eastern Pacific and Indian Oceanand their mutual linkage [R]. Collection of paper abstracts for the 10th seminar on meteorology and climate ineastern Asia and western Pacific [C]. 79-85. |
[7]
|
RASMUSSON E M, CARPENTER T H. Variations in tropical sea surface temperature and surface windfields associated with the southern oscillation/ El Ni?o [J]. Monthly Weather Review, 1982, 111: 517―528. |
[8]
|
ZHANG Zu-qiang, DING Yi-hui, ZHAO Zong-ci. [J]. Acta Meteorologica Sinica, 2000, 58 (1): 11-25. |
[9]
|
DING Yu-guo, JIANG Zhi-hong. Processing of signals from time series of meteorological data [M]. Beijing:Meteorological Press, 1998. 160-167. |
[10]
|
WYRTKI K. El Ni?o El Nino-the dynamic response of the equatorial Pacific Ocean to atmospheric forcing[J]. Journal of Phys. Oceanogr., 1975, 5: 572-584. |
-
-
-