The Dissociation of Oxygen and High Level Circulation in the Atmosphere
Open Access
- 1 May 1964
- journal article
- Published by American Meteorological Society in Journal of the Atmospheric Sciences
- Vol. 21 (3) , 231-237
- https://doi.org/10.1175/1520-0469(1964)021<0231:tdooah>2.0.co;2
Abstract
Ionospheric evidence is presented to show that oxygen at ionospheric heights is dissociated much more in the winter hemisphere than in the summer. The pattern of atmospheric composition is interpreted by a model based on three factors: the dissociation of oxygen, horizontal transport by meridional flow in the upper atmosphere, and vertical transport by diffusion. The second factor introduces large scale meteorology as a major influence in the ionosphere. Abstract Ionospheric evidence is presented to show that oxygen at ionospheric heights is dissociated much more in the winter hemisphere than in the summer. The pattern of atmospheric composition is interpreted by a model based on three factors: the dissociation of oxygen, horizontal transport by meridional flow in the upper atmosphere, and vertical transport by diffusion. The second factor introduces large scale meteorology as a major influence in the ionosphere.Keywords
This publication has 0 references indexed in Scilit: