
The one inch criterion had been use in hail country of the southern plains and over the western United States. Hail is common in these locations due to lower freezing levels in the atmosphere and stronger vertical updrafts. Updrafts result in the formation of hail when water droplets freeze and get carried upward until the they freeze and fall back down. The cycle repetes until the hail grows too large for the updraft to keep it suspended in the air.
This is a good idea because it reduces the perception of over warning saturation during our busy summer storms season. Warnings are often issued for penny sized or 3/4" hail. It is rare for 1" golf ball sized hail to occur in our area. Now thunderstom warnings carry more weight and hopefully people will take them seriously when storms hit.
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