| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 1862017 | Physics Letters A | 2009 | 4 Pages |
Abstract
It is shown that condensation of water vapor produces dynamic instability of atmospheric air and induces air circulation that is characterized by observable air velocities and persists independently of the magnitude of horizontal temperature gradients.
Related Topics
Physical Sciences and Engineering
Physics and Astronomy
Physics and Astronomy (General)
Authors
A.M. Makarieva, V.G. Gorshkov,