On 6 August 2007 a frontal system approached the COPS low-mountain region from the west. In advance of the front, convection initiated along the Vosges Mountains. The storms propagated eastward into the Rhine Valley and produced an outflow boundary that supported secondary initiation.
Dual-Doppler observations were obtained from the Doppler on Wheels (DOW) mobile radars. These systems provided clear-air measurements prior to convection forming in the Vosges Mountains, as well as information about the evolution of the system during its propagation across the Rhine Valley. Additional information about the pre-convective environment will be assessed with the use of surface stations, soundings and GPS moisture retrievals. Comparisons of the observations with high-resolution WRF (Weather Research and Forecasting) simulations will be shown to highlight the necessary features for convective development on this day.
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