Simulation of the Influence of Ion-Produced NOX and HOX Radicals on the Antarctic Ozone Depletion with a One-Dimensional Model

Wang Guiqin

doi:10.1007/BF02919172

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Volume 7 Issue 1

Jan. 1990

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Article > ADVANCES IN ATMOSPHERIC SCIENCES > 1990 > 7(1): 98-103

Simulation of the Influence of Ion-Produced NOX and HOX Radicals on the Antarctic Ozone Depletion with a One-Dimensional Model

Wang Guiqin

1.
Department of Geophysics, Peking University, Beijing 100871

Wang Guiqin

doi: 10.1007/BF02919172

Abstract
References
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Abstract:
A one-dimensional time-dependent photochemical model is used to simulate the influence of ion-produced NOx, and HOx radicals on the Antarctic ozone depletion in polar night and polar spring at a latitude of 73 degrees south.Vertical transport and nitrogen-oxygen (NOx), hydrogen-oxygen (HOx) production by ionic reactions have been introduced into the model.NOx and HOx produced by precipitating ions are transported into the lower stratosphere by vertical motion and have some effects in the development of the Antarctic ozone depletion.From winter through spring the calculated ozone column decreases to 269.4 DU. However, this value is significantly higher than the total ozone observed at several Antarctic ozone stations.
References

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Manuscript History

Manuscript received: 10 January 1990

Manuscript revised: 10 January 1990

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

Simulation of the Influence of Ion-Produced NOX and HOX Radicals on the Antarctic Ozone Depletion with a One-Dimensional Model

Wang Guiqin

1. Department of Geophysics, Peking University, Beijing 100871

Manuscript received: 1990-01-10
Manuscript revised: 1990-01-10

Abstract: A one-dimensional time-dependent photochemical model is used to simulate the influence of ion-produced NOx, and HOx radicals on the Antarctic ozone depletion in polar night and polar spring at a latitude of 73 degrees south.Vertical transport and nitrogen-oxygen (NOx), hydrogen-oxygen (HOx) production by ionic reactions have been introduced into the model.NOx and HOx produced by precipitating ions are transported into the lower stratosphere by vertical motion and have some effects in the development of the Antarctic ozone depletion.From winter through spring the calculated ozone column decreases to 269.4 DU. However, this value is significantly higher than the total ozone observed at several Antarctic ozone stations.