Abstract
The force which acts on an atmospheric vortex depends on its intensity, on the Coriolis parameter and the latitude effect on this parameter. The zonal, meridional and vertical components of this force are linear functions of two correlations: one between the corresponding component of the air velocity and the horizontal divergence of the current and the other, between this same first component and the meridional component of the velocity.
DOI: https://doi.org/10.3402/tellusa.v3i2.8621 | Journal eISSN: 3035-9554
Language: English
Page range: 75 - 77
Published on: Jan 1, 1951
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1951 J. van Mieghem, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.