Therefore, this study develops a comprehensive analysis of precipitation whiplash events on the S2S scale across the contiguous United States between 1915 and 2020. Precipitation whiplash events have been identified by computing the standardized precipitation index (SPI) for 30-day rolling precipitation accumulation totals. A precipitation whiplash occurs at a grid point when the 30-day SPI moves from at or above 1.0 to at or below -1.0, or vice versa. Precipitation whiplash events were then objectively identified, considering the spatial continuity of grid points and implementing independence criteria, to create a database of individual precipitation whiplash events across the contiguous United States at the S2S scale. Using the developed database, events were clustered into regions using k-means clustering so that the climatology of these events and their synoptic drivers could be examined. Overall, we hope that the insights gained from this study will greatly enhance the understanding of precipitation whiplash events across the contiguous United States allowing for better predictability and preparedness into the future.
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