A NOTE ON THE DYNAMICS OF THE QUASI-STATIONARY KUNMING FRONT

CORC > 北京大学 > 地球与空间科学学院

	A NOTE ON THE DYNAMICS OF THE QUASI-STATIONARY KUNMING FRONT
	EGGER, J ; TAO, ZY
刊名	meteorology and atmospheric physics
	1992
DOI	10.1007/BF01029570
英文摘要	The quasi-stationary Kunming front is oriented parallel to the north-south running major mountain chains of south-western China and normal to the upper-level westerlies. The front curves towards the east off the mountain. We hypothesize that the shape of the Kunming front is due to ageostrophic flow along the mountains which is induced by westerly flow in the cold air and at upper levels. Eventually the front must become stagnant. This conjecture is supported by numerical experiments with simple models.; Meteorology & Atmospheric Sciences; SCI(E); 3; ARTICLE; 1-4; 225-229; 48
语种	英语
内容类型	期刊论文
源URL	[http://ir.pku.edu.cn/handle/20.500.11897/258578]
专题	地球与空间科学学院
推荐引用方式 GB/T 7714	EGGER, J,TAO, ZY. A NOTE ON THE DYNAMICS OF THE QUASI-STATIONARY KUNMING FRONT[J]. meteorology and atmospheric physics,1992.
APA	EGGER, J,&TAO, ZY.(1992).A NOTE ON THE DYNAMICS OF THE QUASI-STATIONARY KUNMING FRONT.meteorology and atmospheric physics.
MLA	EGGER, J,et al."A NOTE ON THE DYNAMICS OF THE QUASI-STATIONARY KUNMING FRONT".meteorology and atmospheric physics (1992).