Potential energy of atmospheric water vapor and the air motions induced by water vapor condensation on different spatial scales

Details Potential energy of atmospheric water vapor and the air motions induced by water vapor condensation on different spatial scales Potential energy of atmospheric water vapor and the air motions induced by water vapor condensation on different spatial scales

2010-03-29

arxiv.org/abs/1003.5466v1

Physics

Atmospheric and Oceanic Physics

37 pages, 6 figures

Scientific paper

Basic physical principles are considered that are responsible for the origin of dynamic air flow upon condensation of water vapor, the partial pressure of which represents a store of potential energy in the atmosphere of Earth. Quantitative characteristics of such flow are presented for several spatial scales. It is shown that maximum condensation-induced velocities reach 160 m/s and are realized in compact circulation patterns like tornadoes.

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