Frontolysis

Today, Frontolysis is a topic of great relevance and interest to a wide spectrum of people. With the advancement of technology and globalization, Frontolysis has become a fundamental aspect in the daily lives of many individuals, impacting different aspects such as society, economy, politics and culture. This is why it is essential to delve deeper into the study and analysis of Frontolysis, in order to better understand its influence and impact today. In this article, we will explore different aspects related to Frontolysis, from its historical origin to its implications in the contemporary world, with the aim of providing a comprehensive and updated vision of this very relevant topic.

Frontolysis (also known as Frontal decay) in meteorology, is the dissipation or weakening of an atmospheric front.[1] It is generally described as a decrease in temperature gradients between colliding air masses or can be caused by a shift in wind pattern.[2]

In contrary to areas of "Frontogenesis", the areas where air masses diverge are called areas of frontolysis.

See also

References

  1. ^ Thralls, Zoe A. (1958). The Teaching of Geography. Appleton-Century-Crofts. p. 57. Retrieved 2023-05-13.
  2. ^ "Frontolysis - (Meteorology) - Vocab, Definition, Explanations | Fiveable". library.fiveable.me. Retrieved 2024-10-31.
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