Research Article

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

Table 1

Model options used in this study.

ParametersOptionReferences/comments

ModelWRF-version 3.5.1[20, 21]

Domains d01: 27 km, d02: 9 km, d03: 3 km, d04: 1 kmSee Figure 2(a)

Vertical levels5050 mb top-level pressure, 25 levels below 3 km

Time step 135 secondsA ratio of 3 : 1 was used for nests

Simulation timeStart: 0000 UTC 01 May 2012
End: 0600 UTC 02 May 2012
30 hours; first 18 hours considered as spin-up time

Planetary boundary layerMellor-Yamada-Janjic[22]; successfully used for real-time convective forecasts [23]

Short wave and long wave radiationThe Rapid Radiative Transfer Model (RRTMG) schemes[24]; represent subgrid scale radiative processes