NUMERICAL STUDY OF LAKE-LAND BREEZE OVER LAKE V?TTERN SWEDEN

Wu Zengmao

doi:10.1007/BF02677066

Impact Factor: 5.8

Volume 4 Issue 2

Apr. 1987

Article Contents

Article > ADVANCES IN ATMOSPHERIC SCIENCES > 1987 > 4(2): 198-209

NUMERICAL STUDY OF LAKE-LAND BREEZE OVER LAKE V?TTERN SWEDEN

Wu Zengmao

1.
Shandong College of Oceanology, Qingdao

Wu Zengmao

doi: 10.1007/BF02677066

Abstract
References
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Abstract:
This paper describes a two-dimensional lake breeze model with turbulent energy closure. The simulated results show that (1) the front of the lake breeze progresses inland faster in the late afternoon than at the fully developed stage; and (2) the lake breeze and land breeze have larger extension offshore than inland. The acce-leration of the front in the declining phase of the lake breeze is explained in terms of the decreased turbulent fric-tion acting on the head of the lake breeze. The larger extension offshore, probably, is attributed to the smaller roughness of water surface and to the offshore synoptic wind.
References

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Manuscript History

Manuscript received: 10 April 1987

Manuscript revised: 10 April 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

NUMERICAL STUDY OF LAKE-LAND BREEZE OVER LAKE V?TTERN SWEDEN

Wu Zengmao

1. Shandong College of Oceanology, Qingdao

Manuscript received: 1987-04-10
Manuscript revised: 1987-04-10

Abstract: This paper describes a two-dimensional lake breeze model with turbulent energy closure. The simulated results show that (1) the front of the lake breeze progresses inland faster in the late afternoon than at the fully developed stage; and (2) the lake breeze and land breeze have larger extension offshore than inland. The acce-leration of the front in the declining phase of the lake breeze is explained in terms of the decreased turbulent fric-tion acting on the head of the lake breeze. The larger extension offshore, probably, is attributed to the smaller roughness of water surface and to the offshore synoptic wind.