Understanding Hailstone Temporal Variability and Contributing Factors over the U.S. Southern Great Plains.

J Clim

Earth Systems Science Division, Pacific Northwest National Laboratory, Richland, Washington.

Published: May 2020

AI Article Synopsis

  • * The study analyzed severe hail occurrences in the southern Great Plains from 2004 to 2016 using hail report data and radar-retrieved information, revealing notable year-to-year variability.
  • * The research found that sea surface temperature anomalies in the Gulf of Mexico influence hail variability, with aerosols from northern Mexico showing the strongest correlation to this variability, leading to the recommendation for further studies on aerosol effects.

Article Abstract

Hailstones are a natural hazard that pose a significant threat to property and are responsible for significant economic losses each year in the United States. Detailed understanding of their characteristics is essential to mitigate their impact. Identifying the dynamic and physical factors contributing to hail formation and hailstone sizes is of great importance to weather and climate prediction and policymakers. In this study, we have analyzed the temporal and spatial variabilities of severe hail occurrences over the U.S. southern Great Plains (SGP) states from 2004 to 2016 using two hail datasets: hail reports from the Storm Prediction Center and the newly developed radar-retrieved maximum expected size of hail (MESH). It is found that severe and significant severe hail occurrences have a considerable year-to-year temporal variability in the SGP region. The interannual variabilities have a strong correspondence with sea surface temperature anomalies over the northern Gulf of Mexico and there is no outlier. The year 2016 is identified as an outlier for the correlations with both El Niño-Southern Oscillation (ENSO) and aerosol loading. The correlations with ENSO and aerosol loading are not statistically robust to inclusion of the outlier 2016. Statistical analysis without the outlier 2016 shows that 1) aerosols that may be mainly from northern Mexico have the largest correlation with hail interannual variability among the three factors and 2) meteorological covariation does not significantly contribute to the high correlation. These analyses warrant further investigations of aerosol impacts on hail occurrence.

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Source
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC8097998PMC
http://dx.doi.org/10.1175/jcli-d-19-0606.1DOI Listing

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