Analytic Study of Sea-Land Breezes

K. Young; Zhang Ming

doi:10.1007/BF02973087

Impact Factor: 5.8

Volume 16 Issue 2

Apr. 1999

Article Contents

Article > ADVANCES IN ATMOSPHERIC SCIENCES > 1999 > 16(2): 263-278

Analytic Study of Sea-Land Breezes

1.
Department of Physics, The Chinese University of Hong Kong, Hong Kong, China,LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijng 100080

doi: 10.1007/BF02973087

Abstract
References
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Abstract:
An analytic study of the structure of sea-land breezes is presented, with special attention paid to the dependence on the model parameters. In this linearized model, the wind speed of the sea-land breezes is directly proportional to the difference or sea and land heating rates. For the same differential heating, the sea-land breeze is more prominent if the stratification is weakly stable, or if the frictional force is small. The horizontal penetration from the coast is also investigated, and found to be asymmetric between the land and the sea. The above results are in agreement with observation.
- Sea-land breeze,
- Analytic model
References

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Manuscript History

Manuscript received: 10 April 1999

Manuscript revised: 10 April 1999

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

Analytic Study of Sea-Land Breezes

1. Department of Physics, The Chinese University of Hong Kong, Hong Kong, China,LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijng 100080

Manuscript received: 1999-04-10
Manuscript revised: 1999-04-10

Abstract: An analytic study of the structure of sea-land breezes is presented, with special attention paid to the dependence on the model parameters. In this linearized model, the wind speed of the sea-land breezes is directly proportional to the difference or sea and land heating rates. For the same differential heating, the sea-land breeze is more prominent if the stratification is weakly stable, or if the frictional force is small. The horizontal penetration from the coast is also investigated, and found to be asymmetric between the land and the sea. The above results are in agreement with observation.

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