A unique combination of pre-convective measurements was obtained during COPS with two Doppler on Wheels (DOW) mobile radars and a high-powered water vapor Differential Absorption Lidar (DIAL). The combination of these wind velocity and water vapor measurements in the pre-convective environment may enable better understanding of low-level boundaries in orographic terrain and their associated influence on the distribution of the 3-D moisture field. This is expected to be important for convection initiation applications.
The DIAL and DOW observations will be compared with an ensemble of convection-permitting models, which were available by collaboration with the WWRP Forecast Demonstration Project (FDP) D-PHASE. The comparisons will be performed either with a model forward operator simulating the DOW performance around its site or by profiling of mixing ratio over the DIAL site. Preliminary results indicate that most models suffered from a strong positive moisture bias in the boundary layer, which may have negative implications on their capability to simulate convection initiation. It will be discussed whether these comparisons can be used to investigate the parameterization of land-surface processes and the ABL in atmospheric models.
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