However, the utility of an ensemble clustering technique for convection-allowing ensemble forecast systems remains largely unexplored, mostly due to the prerequisite of an ensemble system of sizable membership for clusters to prove useful. As such, we applied a k-means clustering methodology to a 28-member time-lagged Rapid Refresh Forecast System ensemble (RRFSe) system for the 2024 Hydrometeorology Testbed (HMT) Flash Flood and Intense Rainfall (FFaIR) experiment. Four clusters were computed daily from the full ensemble 6-h QPF field within a floater domain. Participants had the clustering output at their disposal for forecast purposes, and on the subsequent day, participants were asked to subjectively evaluate the performance of the clusters relative to observed precipitation accumulation and the full ensemble QPF field. 83.7% of responses during the experiment indicated that at least one of the 75th percentile QPF clusters outperformed the full ensemble 75th percentile QPF. When asked if the clusters simply grouped membership by initialization time, participants unanimously responded that different cycle times were well-represented amongst the clusters. This result not only bodes well for viability of the clustering approach on a time-lagged RRFSe, but also suggests that time-lagging could be a viable source of useful ensemble spread in future iterations of the RRFS ensemble system. These results and more insights gained from participants of the 2024 HMT FFaIR experiment will be discussed.
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