The Weather Research and Forecasting (WRF) model will be used to simulate this event. The ability of the WRF boundary- and surface-layer schemes to properly represent the atmosphere above complex orography is not well understood, however: sensitivities are known to exist, which is unsurprising given the large degree of freedom in choosing physical parametrisations. For this study, the sensitivity tests are restricted to those which directly affect the boundary layer specification.
From the group of simulations, and via comparison with observational data such as radiosondes, the potential problems in the available boundary layer schemes (such as boundary layers being too well-mixed)will be demonstrated. The importance of a good representation of soil moisture will also be shown. Out of all the tests performed for this case, only one run produced results which bore resemblance to the observed cloud (indeed, the remaining runs did not produce any cloud at all). The modelled structure of the boundary layer, and specification of surface moisture, are seen to be of crucial importance.
This study has important implications for the forecasting of deep convective clouds in complex terrain - and for convection in general - and illustrates the important physical processes which need to be adequately represented for a realistic model simulation.