Geoscientific Model Development
Geoscientific Model Development
GMD
Articles | Volume 11, issue 5
Articles | Volume 11, issue 5
https://doi.org/10.5194/gmd-11-1785-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-11-1785-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 11, issue 5
Methods for assessment of models
 | 
08 May 2018
Methods for assessment of models |  | 08 May 2018

Impacts of the horizontal and vertical grids on the numerical solutions of the dynamical equations – Part 2: Quasi-geostrophic Rossby modes

Celal S. Konor and David A. Randall

Viewed

Total article views: 2,358 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,523 738 97 2,358 349 79 120
  • HTML: 1,523
  • PDF: 738
  • XML: 97
  • Total: 2,358
  • Supplement: 349
  • BibTeX: 79
  • EndNote: 120
Views and downloads (calculated since 22 Dec 2017)
Cumulative views and downloads (calculated since 22 Dec 2017)

Viewed (geographical distribution)

Total article views: 2,358 (including HTML, PDF, and XML) Thereof 2,224 with geography defined and 134 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 04 Feb 2025
Download
Short summary
We have discussed the effects of discretization on dispersion of midlatitude Rossby waves on the A, B, C, CD, (DC), D, E and Z horizontal grids, and the L and CP vertical grids. The Z, C, D and CD (DC) grids generate similar dispersion of the baroclinic and barotropic Rossby modes. The A, E and B grids generate multiple (non-unique) solutions. The modes with the smallest resolvable vertical scale on the L grid do not retrograde. The CP-grid solutions are much more accurate than the L grid.
Read more
Share