While details in the location and amounts of an extreme precipitation event like this are difficult to predict as a slight misplacement of the synoptic and mesoscale features by the numerical models that drive the strongest convective thunderstorms, a meteorologist can detect and communicate the possibility of this occurring. For this event, high-resolution models, including the HRRR and a WRF-ARW model run locally by the National Weather Service in San Diego, showed local hourly rainfall amounts of 50 mm or more in one hour up to 36 hours in advance of the rainfall, though not in the exact location. Ensemble models, including ENS, also showed the potential for very high rainfall amounts, including 95th percentile values as high as 125 mm for a 12-hour period over San Diego on 22 Jan 2024 from the ensemble run issued 24 hours in advance. As a result, meteorologists at the National Weather Service Forecast Office in San Diego were able to issue a flood watch the day before the event and produce messaging for emergency managers and other National Weather Service partners mentioning a risk of heavy rain five days before the event. Operational meteorologists creating forecasts and impact-based decision support services need to identify the weather elements creating major events like this which result in around 1000 homes damaged or destroyed and an estimated $90 million of damage.
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