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

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