WAVE BOUNDARY BETWEEN MIDDLE-AND-LOW AND MIDDLE-AND-HIGH LATITUDE CIRCULATIONS, AND SEASONAL TRANSFORMATION OF NORTHERN-HEMISPHERE MEAN CIRCULATION

Wang Panxing; Liu Dai; Pan Deyu

doi:10.1007/BF02656661

Impact Factor: 5.8

Volume 4 Issue 1

Jan. 1987

Article Contents

Article > ADVANCES IN ATMOSPHERIC SCIENCES > 1987 > 4(1): 55-65

WAVE BOUNDARY BETWEEN MIDDLE-AND-LOW AND MIDDLE-AND-HIGH LATITUDE CIRCULATIONS, AND SEASONAL TRANSFORMATION OF NORTHERN-HEMISPHERE MEAN CIRCULATION

1.
Nanjing Institute of Meteorology, Nanjing,Nanjing Institute of Meteorology, Nanjing,Nanjing Institute of Meteorology, Nanjing

doi: 10.1007/BF02656661

Abstract
References
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Abstract:
The definition Tor stability D of standing waves given in this paper is used to denote the relative magnitude of annual variation of the waves. Analysis of the temporal (seasonal) and spatial (meridional) changes of the monthly mean circulation at 500 and 100 hPa shows its temporal and spatial demarcation and the bourdary be-tween the middle-and-low latitude circulation and the middle-aod-high latitude circulation in the wave field. Based on the annual march of D and the position of the boundary, a discussion is made of the seasonal trans-formation of the Northern- Hemisphere mean circulation and Ihe- pattern of its development.
References

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Manuscript History

Manuscript received: 10 January 1987

Manuscript revised: 10 January 1987

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

WAVE BOUNDARY BETWEEN MIDDLE-AND-LOW AND MIDDLE-AND-HIGH LATITUDE CIRCULATIONS, AND SEASONAL TRANSFORMATION OF NORTHERN-HEMISPHERE MEAN CIRCULATION

1. Nanjing Institute of Meteorology, Nanjing,Nanjing Institute of Meteorology, Nanjing,Nanjing Institute of Meteorology, Nanjing

Manuscript received: 1987-01-10
Manuscript revised: 1987-01-10

Abstract: The definition Tor stability D of standing waves given in this paper is used to denote the relative magnitude of annual variation of the waves. Analysis of the temporal (seasonal) and spatial (meridional) changes of the monthly mean circulation at 500 and 100 hPa shows its temporal and spatial demarcation and the bourdary be-tween the middle-and-low latitude circulation and the middle-aod-high latitude circulation in the wave field. Based on the annual march of D and the position of the boundary, a discussion is made of the seasonal trans-formation of the Northern- Hemisphere mean circulation and Ihe- pattern of its development.