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

<div>Surface (2 m) WRF simulation for 1 May 2012. (a) Water vapor mixing ratio (g/kg) and wind stream lines valid at 1900 UTC. (b) Temperature (degree Celsius) valid at 1700 UTC.</div>

Advances in Meteorology

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Figure 5

Figure 5: Numerical Simulations of the 1 May 2012 Deep Convection Event over Cuba: Sensitivity to Cumulus and Microphysical Schemes in a High-Resolution Model 

Figure 5 | Numerical Simulations of the 1 May 2012 Deep Convection Event over Cuba: Sensitivity to Cumulus and Microphysical Schemes in a High-Resolution Model 