EGU26-2009, updated on 13 Mar 2026
https://doi.org/10.5194/egusphere-egu26-2009
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Tuesday, 05 May, 16:15–18:00 (CEST), Display time Tuesday, 05 May, 14:00–18:00
 
Hall X5, X5.3
New mountain-generated mesoscale flow test cases from DCMIP2025
Timothy Andrews1, Christiane Jablonowski1, Owen Hughes1, and Thomas Bendall2
Timothy Andrews et al.
  • 1University of Michigan, Climate and Space Sciences, United States of America
  • 2Dynamics Research, Met Office, Exeter, United Kingdom

The Dynamical Core Intercomparison Project (DCMIP) is an endeavour to evaluate and compare dynamical cores through the application of idealised test cases. Previous editions of DCMIP, in 2008, 2012, and 2016, introduced many widely used cases, including baroclinic wave, tracer transport, supercell, and tropical cyclone tests. We present a new test case developed for the most recent edition of DCMIP, held in June 2025 (DCMIP2025). This case uses an easily implementable initial condition, with the addition of mountain orography, to generate nonlinear mesoscale flow phenomena. Two different orographies are considered, which lead to dynamics of a gap flow and vortex shedding. The gap flow case exhibits accelerated flow and the creation of a pair of symmetric lee vortices, whilst the vortex shedding case instigates a flow reminiscent of a von Kármán vortex street. These tests are compared in four dynamical cores: three from the United States, along with GungHo, the compatible finite element dynamical core from the UK Met Office’s new LFRic model. Contrasting simulations with each dynamical core highlights differences in the numerical designs, including the grid choice and sources of numerical diffusion.

How to cite: Andrews, T., Jablonowski, C., Hughes, O., and Bendall, T.: New mountain-generated mesoscale flow test cases from DCMIP2025, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-2009, https://doi.org/10.5194/egusphere-egu26-2009, 2026.