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EGU2013-2876.pdf

EGU2013-2876.pdf
Preview of EGU2013-2876
🔗 Source: meetingorganizer.copernicus.org
📊 Size: 34 KB
📄 Pages: 1 page
⬇️ Downloads: 79

Summary

Global models struggle to represent the West African Monsoon water cycle, with poor representations of deep convection's diurnal cycle and organisation. Convection-permitting simulations using the Met Office Unified Model provide a more realistic distribution and diurnal cycle of convection, significantly impacting the mean Sahel-Sahara pressure gradient and monsoon flow. Explicit convection improves rainfall totals, with increased evapotranspiration compensated by moisture flux convergence, creating self-sustaining heavier Sahel rains that interact with the monsoon flow to bring more moisture into the region.

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Description

Global models struggle to represent the West African Monsoon water cycle, with poor representations of deep convection's diurnal cycle and organisation.

Technical Information

  • File Format: PDF
  • File Size: 34 KB
  • Pages: 1
  • Language: EN
  • Total Downloads: 79
  • Last Updated: 1 week ago

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