Geoscientific Model Development
Geoscientific Model Development
GMD
Articles | Volume 11, issue 5
Articles | Volume 11, issue 5
https://doi.org/10.5194/gmd-11-1753-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-11-1753-2018
© 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 1: Nonhydrostatic inertia–gravity modes

Celal S. Konor and David A. Randall

Viewed

Total article views: 3,003 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,934 976 93 3,003 390 105 127
  • HTML: 1,934
  • PDF: 976
  • XML: 93
  • Total: 3,003
  • Supplement: 390
  • BibTeX: 105
  • EndNote: 127
Views and downloads (calculated since 22 Dec 2017)
Cumulative views and downloads (calculated since 22 Dec 2017)

Viewed (geographical distribution)

Total article views: 3,003 (including HTML, PDF, and XML) Thereof 2,843 with geography defined and 160 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 02 Apr 2025
Download
Short summary
We have discussed the discretizations of the three-dimensional nonhydrostatic linearized anelastic equations on the A, B, C, CD, (DC), D, E and Z horizontal grids, and on the L and CP vertical grids, with an emphasis on midlatitude inertia–gravity waves. The Z and C grids show the most accurate dispersion among the seven horizontal grids. The inertia–gravity mode solutions with the D and CD grids are almost identical. The A, B and E grids suffer from the multiple (or non-unique) physical modes.
Read more
Share