Articles | Volume 15, issue 19
https://doi.org/10.5194/gmd-15-7471-2022
https://doi.org/10.5194/gmd-15-7471-2022
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

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Latest update: 17 Jun 2024
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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.