The storm's updraft, with upwardly directed wind speeds as higher as a hundred and ten mph (a hundred and eighty km/h),[thirteen] blows the forming hailstones up the cloud. Given that the hailstone ascends, it passes into areas of the cloud where by the concentration of humidity and supercooled water droplets https://elliotsyejp.mappywiki.com/838969/rumored_buzz_on_thornton