A very strong sand-dust storm occurred on 5 May, 1993 in Northwest China. In order to give a detailed description of the evolution of a mesoscale system along with the heavy sand-dust storm, a complex model including improved physicalprocesses and a radiation parameterization scheme was developedbased on a simulation model. The improved model introduced a sand-dust transport equation as well as a lifting transportmodel, sand-dust aerosols and radiation parameterization scheme.Using this model, the super sand-dust storm case on 5 May was simulated. Results indicated that the coupled mesoscale model successfully simulated the mesoscale vortex, its strong upwardmovement and the warm core structure of PBL. The generation anddevelopment of these structures were consistent with that of the sand-dust storm and dry squall-line (which was different withnormal squall-line). Simulated sand-dust concentration and its radiative effect corresponded with observation data. The radiative effect of sand-dust aerosols caused the air to heat on the top of aerosol layer with a heating rate amounting to 2 K hr-1. As a result, solar radiation flux that reached the surface, netradiation flux and surface temperature all suddenly went down. The temperature gradient across the cold front became obviouslylarger. Therefore, enhancing the development of the mesoscalesystem. The simulation generally reflected features during thesquall-line passage of this strong sand-dust storm.
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Zhang, XL., Cheng, L. & Chung, YS. Development of a Severe Sand-dust Storm Model and its Application to Northwest China. Water, Air, & Soil Pollution: Focus 3, 173–190 (2003). https://doi.org/10.1023/A:1023290408545
- mesoscale system
- model improvement
- sand-dust storm