what are the factors that are favoring it?
Movement of dry air into strong thunderstorms over continents can increase the frequency of hail by promoting evaporational cooling which lowers the freezing level of thunderstorm clouds giving hail a larger volume to grow in.
Hail
Hail is most common within continental interiors of the mid-latitudes, as hail formation is considerably more likely when the freezing level is below the altitude of . Movement of dry air into strong thunderstorms over continents can increase the frequency of hail by promoting evaporational cooling which lowers the freezing level of thunderstorm clouds giving hail a larger volume to grow in. Accordingly, hail is less common in the tropics despite a much higher frequency of thunderstorms than in the mid-latitudes because the atmosphere over the tropics tends to be warmer over a much greater altitude. Hail in the tropics occurs mainly at higher elevations.
what is a common feature of many weather systems responsible for floods in north america Due to a thunderstorm can you describe its life cycle? The developing stage - masses of moisture are lifted upwards into the atmosphere;  the mature stage - the warmed air continues to rise until it reaches an area of warmer air and can rise no farther; and the dissipation stage - downbursts. are they classified? Yes - single-cell, multi-cell, squall line (also called multi-cell line) and supercell thunderstorms what is hail? A form of solid precipitation. It consists of balls or irregular lumps of ice, each of which is called a hailstone. how is it formed? In strong thunderstorm clouds - particularly those with intense updrafts, high liquid water content, great vertical extent, large water droplets, and where a good portion of the cloud layer is below freezing .
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Hail [SEP] Factors favoring hail
Hail is most common within continental interiors of the mid-latitudes, as hail formation is considerably more likely when the freezing level is below the altitude of . Movement of dry air into strong thunderstorms over continents can increase the frequency of hail by promoting evaporational cooling which lowers the freezing level of thunderstorm clouds giving hail a larger volume to grow in. Accordingly, hail is less common in the tropics despite a much higher frequency of thunderstorms than in the mid-latitudes because the atmosphere over the tropics tends to be warmer over a much greater altitude. Hail in the tropics occurs mainly at higher elevations.