Numerical Modelling of the Effects of Ozone on the Summer Atmospheric Circulation

Wang Qianqian; Wang Yinhui; Song Yu; Qian Yongfu

doi:10.1007/BF02666546

Impact Factor: 5.8

Volume 11 Issue 2

Apr. 1994

Article Contents

Article > ADVANCES IN ATMOSPHERIC SCIENCES > 1994 > 11(2): 201-211

Numerical Modelling of the Effects of Ozone on the Summer Atmospheric Circulation

1.
Nanjing Institute of Meteorology, Nanjing 210044,Nanjing Institute of Meteorology, Nanjing 210044,Nanjing Institute of Meteorology, Nanjing 210044,Department of Atmospheric Sciences, Nanjing University, Nanjing 210008

doi: 10.1007/BF02666546

Abstract
References
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Abstract:
The effects of ozone on the summer atmospheric general circulation are simulated by use of a zonal model with the p-sigma coordinate system. Results show that the simulated properties at the upper levels are remarkably im-proved after the ozone effects are introduced to the model. The direct effect of ozone is to enhance the heating rates at the upper levels. In the lower atmosphere, this effect is very little. Furthermore, the ozone can change the distributions and values of other components of heating fields, resulting in the change of the total heating rates, and meanwhile induce evident variation of atmospheric circulation at the lower levels.
- Ozone and radiation,
- Numerical modelling of atmospheric circulation,
- Atmospheric heating field
References

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Manuscript History

Manuscript received: 10 April 1994

Manuscript revised: 10 April 1994

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 Modelling of the Effects of Ozone on the Summer Atmospheric Circulation

1. Nanjing Institute of Meteorology, Nanjing 210044,Nanjing Institute of Meteorology, Nanjing 210044,Nanjing Institute of Meteorology, Nanjing 210044,Department of Atmospheric Sciences, Nanjing University, Nanjing 210008

Manuscript received: 1994-04-10
Manuscript revised: 1994-04-10

Abstract: The effects of ozone on the summer atmospheric general circulation are simulated by use of a zonal model with the p-sigma coordinate system. Results show that the simulated properties at the upper levels are remarkably im-proved after the ozone effects are introduced to the model. The direct effect of ozone is to enhance the heating rates at the upper levels. In the lower atmosphere, this effect is very little. Furthermore, the ozone can change the distributions and values of other components of heating fields, resulting in the change of the total heating rates, and meanwhile induce evident variation of atmospheric circulation at the lower levels.

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