Abstract
A two-parameter geostrophic model is described. Primary emphasis is placed on the integration scheme used. This scheme implies computation of trajectories and interpolation of vorticity and a certain function of thickness in the endpoints of the trajectories.
DOI: https://doi.org/10.3402/tellusa.v15i3.8844 | Journal eISSN: 3035-9554
Language: English
Page range: 280 - 283
Published on: Jan 1, 1963
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1963 Hans Økland, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.