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.
- ^ Thralls, Zoe A. (1958). The Teaching of Geography. Appleton-Century-Crofts. p. 57. Retrieved 2023-05-13.
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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.
- ^ Thralls, Zoe A. (1958). The Teaching of Geography. Appleton-Century-Crofts. p. 57. Retrieved 2023-05-13.
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| This meteorology–related article is a stub. You can help Wikipedia by expanding it. |