This study utilizes data collected by the airborne University of Wyoming Cloud Radar (WCR) aboard the NCAR/NSF C-130 in the comma head of three cyclones observed during PLOWS. The high 15 m resolution of the WCR allows the detection of mesoscale circulations such as the several kilometer deep convective updrafts of up to 5 ms-1 within the upper level dry intrusion, as well as the smaller scale cloud top generating cells with horizontal sizes ranging from 0.5 to 1.5 km and vertical motions in excess of 1 ms-1. In this presentation, data from the operational Rapid Update Cycle (RUC) model is used in conjunction with WCR data to show how reduced stability above the warm front leads to the growth of the deep convection within the dry intrusion, and to cloud top generating cells. We relate the transverse frontogenesis circulation to the larger scale precipitation morphology. Finally, contour frequency by altitude diagrams (CFADs) are used to show that much of the precipitation outside of the dry slot convection and the generating cells is falling near its terminal velocity, indicating a lack of significant broad-scale vertical motion within the stratiform regions.