Geoscientific Model Development
Geoscientific Model Development
GMD
Articles | Volume 15, issue 19
Articles | Volume 15, issue 19
https://doi.org/10.5194/gmd-15-7471-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-15-7471-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 15, issue 19
Model evaluation paper
 | 
10 Oct 2022
Model evaluation paper |  | 10 Oct 2022

Tropospheric transport and unresolved convection: numerical experiments with CLaMS 2.0/MESSy

Paul Konopka, Mengchu Tao, Marc von Hobe, Lars Hoffmann, Corinna Kloss, Fabrizio Ravegnani, C. Michael Volk, Valentin Lauther, Andreas Zahn, Peter Hoor, and Felix Ploeger

Viewed

Total article views: 1,452 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,158 269 25 1,452 16 9
  • HTML: 1,158
  • PDF: 269
  • XML: 25
  • Total: 1,452
  • BibTeX: 16
  • EndNote: 9
Views and downloads (calculated since 18 May 2022)
Cumulative views and downloads (calculated since 18 May 2022)

Viewed (geographical distribution)

Total article views: 1,452 (including HTML, PDF, and XML) Thereof 1,354 with geography defined and 98 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 24 Sep 2023
Download
Short summary
Pure trajectory-based transport models driven by meteorology derived from reanalysis products (ERA5) take into account only the resolved, advective part of transport. That means neither mixing processes nor unresolved subgrid-scale advective processes like convection are included. The Chemical Lagrangian Model of the Stratosphere (CLaMS) includes these processes. We show that isentropic mixing dominates unresolved transport. The second most important transport process is unresolved convection.
Read more