Abstract:
Regular features of motion of thermics in a stratified atmosphere are considered. Thermics are single and multiple free volumes of floating gas, which successively arise with a certain frequency near a horizontal surface. In a real atmosphere, large-scale thermics of this type appear, for example, as a result of powerful pulse actions on the ambient medium that are successively produced at one point near the Earth surface.
Citation:
B. I. Zaslavskii, B. V. Yur'ev, “Motion of thermics in a stratified atmosphere”, Prikl. Mekh. Tekh. Fiz., 40:5 (1999), 33–39; J. Appl. Mech. Tech. Phys., 40:5 (1999), 805–810
This publication is cited in the following 1 articles:
A. A. Spivak, Yu. S. Rybnov, S. A. Riabova, S. P. Soloviev, V. A. Kharlamov, “Acoustic, Magnetic, and Electric Effects of Stromboli Volcano Eruption, Italy, in July–August 2019”, Izv., Phys. Solid Earth, 56:5 (2020), 708