An example of a high-impact precipitation event occurred over Wake County on the 4th of July holiday in 2001, producing flash flooding, frequent lightning and up to 6 inches of rain. This event was not accurately predicted by numerical models and it had major impacts on the public, as people were caught outdoors and unprepared at holiday events. The objectives of studying such a significant, high-impact event were to understand the basic factors that resulted in such focused, heavy convection. It was determined that the focus for heavy thunderstorm activity was related to a cold front, a sea breeze, environmental instability, outflow boundaries that propagated convection, and the presence of other surface-driven/mesoscale boundaries. Additionally, observations, model output, and sensitivity test results were examined in order to identify signatures that can alert forecasters to flash flood potential in the future, even when model QPF guidance is lacking.
Results reveal that because it is highly unlikely that a numerical model can represent such a focused and rare event, forecasters must instead look to observations and environmental factors that possibly signal flash flooding, even in the absence of trustworthy model QPF guidance.
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