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Abstract
Composite investigation is performed of global dynamic characteristics of 3-4-year period low-frequency oscillation in ENSO variability of air-sea coupling in the context of monthly mean wind and SSTA.Evidence suggests that the horizontal(vertical) anomaly circulation at tropical latitudes (equatorial)exhibits their evolution to be,in substance,a kind of low-frequency wave slowly travelling eastward,featured by wave number 2 moving along the equator and zonal wind swiftly decaying off the equator in relation to divergence/convergence:the time that the low-frequency wave takes to move around the equator in its halfway is precisely the period of the ENSO low-frequency component (LFC) (approximately 4 years);the ocean also displays corresponding response to the component.
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Citation
Zou Li, Ni Yunqi. 1996: DIAGNOSIS OF LOW FREQUENCY COMPONENT OF ENSO VARIABILITY-PART Ⅰ:GLOBAL-SCALE DYNAMIC CHARACTERISTICS OF THE COMPONENT. Journal of Meteorological Research, 10(4): 419-429.
Zou Li, Ni Yunqi. 1996: DIAGNOSIS OF LOW FREQUENCY COMPONENT OF ENSO VARIABILITY-PART Ⅰ:GLOBAL-SCALE DYNAMIC CHARACTERISTICS OF THE COMPONENT. Journal of Meteorological Research, 10(4): 419-429.
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Zou Li, Ni Yunqi. 1996: DIAGNOSIS OF LOW FREQUENCY COMPONENT OF ENSO VARIABILITY-PART Ⅰ:GLOBAL-SCALE DYNAMIC CHARACTERISTICS OF THE COMPONENT. Journal of Meteorological Research, 10(4): 419-429.
Zou Li, Ni Yunqi. 1996: DIAGNOSIS OF LOW FREQUENCY COMPONENT OF ENSO VARIABILITY-PART Ⅰ:GLOBAL-SCALE DYNAMIC CHARACTERISTICS OF THE COMPONENT. Journal of Meteorological Research, 10(4): 419-429.
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