Numerical Simulations of the 1 May 2012 Deep Convection Event over Cuba: Sensitivity to Cumulus and Microphysical Schemes in a High-Resolution Model

<div>Era Interim data valid for 1800 UTC on 1 May 2012. (a) Sea level pressure (shaded) and wind field (barbs) at 850 mb. (b) Vorticity (shaded) and wind field (barbs) at 200 mb. The brown line over the Gulf of Mexico in (a) represents a trough.</div>

Advances in Meteorology

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Figure 3

Figure 3: Numerical Simulations of the 1 May 2012 Deep Convection Event over Cuba: Sensitivity to Cumulus and Microphysical Schemes in a High-Resolution Model 

Figure 3 | Numerical Simulations of the 1 May 2012 Deep Convection Event over Cuba: Sensitivity to Cumulus and Microphysical Schemes in a High-Resolution Model 