Abstract
Approximations in the use of any scalar dependent variable as a vertical coordinate in Dynamic Meteorology are derived. A connection with the barotropic approximation is made for the case of a pressure coordinate system where the dependent variable is pressure.
DOI: https://doi.org/10.3402/tellusa.v16i1.8890 | Journal eISSN: 3035-9554
Language: English
Page range: 26 - 31
Published on: Jan 1, 1964
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1964 T. M. L. Wigley, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.