Category:Meteorological inversion

In meteorology, an inversion is a deviation from the normal change of an atmospheric property with altitude. It almost always refers to a temperature inversion, i.e., an increase in temperature with height, or to the layer (inversion layer) within which such an increase occurs.

Subcategories

This category has the following 2 subcategories, out of 2 total.

F

M

Pages in category "Meteorological inversion"

This category contains only the following page.

Media in category "Meteorological inversion"

The following 52 files are in this category, out of 52 total.

Last modified on 26 January 2012, at 15:38