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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.


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



Pages in category "Meteorological inversion"

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Media in category "Meteorological inversion"

The following 179 files are in this category, out of 179 total.