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Evolution mechanism of the western Pacific subtropical high

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Science in China Series D: Earth Sciences : Volume 46, Issue 1, Supplement,March 2003

Science in China Series D: Earth Sciences : Volume 46, Issue 2, February 2003

Science in China Series D: Earth Sciences : Volume 46, Issue 2, Supplement,February 2003

Science in China Series D: Earth Sciences : Volume 45

Science in China Series D: Earth Sciences : Volume 44

Science in China Series D: Earth Sciences : Volume 43

Science in China Series D: Earth Sciences : Volume 42

Science in China Series D: Earth Sciences : Volume 41

Science in China Series D: Earth Sciences : Volume 40

Evolution mechanism of the western Pacific subtropical high

Content Provider	Springer Nature Link
Author	Cao, Jie Huang, Ronghui Xie, Yingqi Tao, Yun
Copyright Year	2003
Abstract	To surmount the deficiency in studying the multiple equilibrium states in the atmosphere motion with highly truncated spectral method, the trigonometric functions for describing the prototypical 500 hPa height fields and the outgoing long wave radiation (OLR) fields are retrieved respectively for the northward bias and the southward bias years of the western Pacific subtropical high with corresponding observational data and the optimum subset retrieval method for four factors. Then the evolution mechanism of the western Pacific subtropical high is studied by means of multiple equilibrium state theory. The results show that the cause of inducing the abnormal location of the western Pacific subtropical high is differences in the early external thermal forcing, which evoke different waveforms in atmosphere. If the early meridional and zonal external thermal forcing differences are stronger, there are wave-mean flow and wave-wave interactions between the response waveforms in atmosphere. In such a case, the western Pacific subtropical high shifts northward obviously. On the contrary, when the early meridional and zonal external thermal forcing differences are weaker, there is no wave-mean flow interaction between the response waveforms in atmosphere, and accordingly the position of the western Pacific subtropical high oscillates with the external thermal forcing oscillation, and is on the south of normal.
Starting Page	257
Ending Page	268
Page Count	12
File Format	PDF
ISSN	10069313
Journal	Science in China Series D: Earth Sciences
Volume Number	46
Issue Number	3
e-ISSN	18622801
Language	English
Publisher	Science in China Press
Publisher Date	2003-01-01
Publisher Place	Beijing
Access Restriction	Subscribed
Subject Keyword	western Pacific subtropical high wave-mean flow interaction highly truncated spectral method multiple equilibrium state Geosciences
Content Type	Text
Resource Type	Article
Subject	Earth and Planetary Sciences

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