The storm's updraft, with upwardly directed wind speeds as superior as a hundred and ten mph (a hundred and eighty km/h),[13] blows the forming hailstones up the cloud. Given that the hailstone ascends, it passes into areas of the cloud exactly where the concentration of humidity and supercooled water droplets https://plumbing-mep64207.buscawiki.com/839961/detailed_notes_on_thornton