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.
| Parameters | Option | References/comments |
| Model | WRF-version 3.5.1 | [20, 21] |
| Domains | d01: 27 km, d02: 9 km, d03: 3 km, d04: 1 km | See Figure 2(a) |
| Vertical levels | 50 | 50 mb top-level pressure, 25 levels below 3 km |
| Time step | 135 seconds | A ratio of 3 : 1 was used for nests |
| Simulation time | Start: 0000 UTC 01 May 2012 End: 0600 UTC 02 May 2012 | 30 hours; first 18 hours considered as spin-up time |
| Planetary boundary layer | Mellor-Yamada-Janjic | [22]; successfully used for real-time convective forecasts [23] |
| Short wave and long wave radiation | The Rapid Radiative Transfer Model (RRTMG) schemes | [24]; represent subgrid scale radiative processes |
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