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surface of a snowpack when temperatures get above freezing for a period of time and melt the surface snow. Once temperatures return to below freezing, the melted snow re-freezes into a firm crust. Thicker, stronger melt-freeze crusts develop when the process continues for several days. During springtime, solar radiation on a slope also accelerates the melting process during the day and forms a sun crust once temperatures cool below freezing overnight. Hailis precipitation in the form of hard pellets of ice and only forms in cumulonimbus clouds where the lower region of the cloud contains liquid water and is above freezing, while the upper region is below Trending viking fathor all over printed air jordan 13 sneakersfreezing. When an ice pellet falls within the cumulonimbus cloud, it enters the warm, liquid region and picks up moisture. Then the updrafts through the ice pellet back up above the freezing point hardening the newly gathered water. The ice pellet will fall again to collect liquid water and thrown back up to refreeze. This process will continue until the weight of the hail stone becomes to heavy for the updrafts to hold it up. Once the hail becomes too heavy, the hail will precipitate from the cloud. Snowis precipitation in the form of ice crystals. The size, shape and concentration of snowflakes depends on

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