4.7 Article

A Pan-African Convection-Permitting Regional Climate Simulation with the Met Office Unified Model: CP4-Africa

Journal

JOURNAL OF CLIMATE
Volume 31, Issue 9, Pages 3485-3508

Publisher

AMER METEOROLOGICAL SOC
DOI: 10.1175/JCLI-D-17-0503.1

Keywords

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Funding

  1. Natural Environment Research Council/Department for International Development via the Future Climate for Africa (FCFA) [NE/M017214/1, NE/M017230/1]
  2. Natural Environment Research Council [NE/M017230/1, NE/R016518/1, NE/M017214/1, nceo020006] Funding Source: researchfish
  3. NERC [NE/M017230/1, nceo020006, NE/M017214/1] Funding Source: UKRI

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A convection-permitting multiyear regional climate simulation using the Met Office Unified Model has been run for the first time on an Africa-wide domain. The model has been run as part of the Future Climate for Africa (FCFA) Improving Model Processes for African Climate (IMPALA) project, and its configuration, domain, and forcing data are described here in detail. The model [Pan-African Convection-Permitting Regional Climate Simulation with the Met OfficeUM(CP4-Africa)] uses a 4.5-km horizontal grid spacing at the equator and is run without a convection parameterization, nested within a global atmospheric model driven by observations at the sea surface, which does include a convection scheme. An additional regional simulation, with identical resolution and physical parameterizations to the global model, but with the domain, land surface, and aerosol climatologies of CP4-Africa, has been run to aid in the understanding of the differences between the CP4-Africa and global model, in particular to isolate the impact of the convection parameterization and resolution. The effect of enforcing moisture conservation in CP4-Africa is described and its impact on reducing extreme precipitation values is assessed. Preliminary results from the first five years of the CP4-Africa simulation show substantial improvements in JJA average rainfall compared to the parameterized convection models, with most notably a reduction in the persistent dry bias in West Africa, giving an indication of the benefits to be gained from running a convection-permitting simulation over the whole African continent.

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