Frontolysis in meteorology, is the dissipation or weakening of an atmospheric front. [1]
In contrary to areas of " Frontogenesis", the areas where air masses diverge are called areas of frontolysis.
See also
References
- ^ Thralls, Zoe A. (1958). The Teaching of Geography. Appleton-Century-Crofts. p. 57. Retrieved 2023-05-13.
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