On the numerical solution of diabatic quasi-geostrophic Omega equation

Authors

  • J. SHUKLA Institute of Tropical Meteorology, Poona

DOI:

https://doi.org/10.54302/mausam.v22i1.3981

Abstract

The quasi-geostrophic omega equation has been numerically solved to get the vertical velocity distribution in a typical westerly disturbance. The effects of sensible heat and latent heat of condensation are also for a 4-layer model. The computations were performed on HITAC 5020.

The numerically obtained vertical velocity field is in good agreement with the observed weather pattern associated with the middle latitude large-scale disturbance, i.e., ascending motion in front of the trough and downward motion in the rear of the trough.

Downloads

Published

01-01-1971

How to Cite

[1]
J. . SHUKLA, “On the numerical solution of diabatic quasi-geostrophic Omega equation”, MAUSAM, vol. 22, no. 1, pp. 35–46, Jan. 1971.

Issue

Vol. 22 No. 1 (1971): MAUSAM

Section

Research Papers

License

Copyright (c) 2021 MAUSAM

Creative Commons License

This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.

All articles published by MAUSAM are licensed under the Creative Commons Attribution 4.0 International License. This permits anyone.

Anyone is free:

  • To Share - to copy, distribute and transmit the work
  • To Remix - to adapt the work.

Under the following conditions:

  • Share - copy and redistribute the material in any medium or format
  • Adapt - remix, transform, and build upon the material for any purpose, even
    commercially.