This study examines the impact of assimilating ZDR-derived PBL depth observations on the forecasts of the flash flooding event happened in east Kentucky in July 2022. The model configuration in the experiments mimics the operational HRRR. Results show that assimilating ZDR-derived PBL depth observations led to considerable changes in temperature and moisture in the lower troposphere. Soil conditions, including soil moisture, and associated surface heat fluxes, are also modified. These impacts of assimilating ZDR-derived PBL depth observations contribute to a better match between model-diagnosed PBL depth with the observations. Subsequently, rainfall forecasts are statistically significantly improved for multiple different thresholds using both grid-wise and neighborhood metrices, especially for the most extreme rainfall. Sensitivity experiments also show that the assimilation frequency and the observation errors assigned to ZDR-derived PBL depth observations also influence the performance of the rainfall forecasts, which deserves future studies to explore more adaptive methods.
- Indicates paper has been withdrawn from meeting
- Indicates an Award Winner