Snowpack conditions in Alabama are generally limited, as the state experiences a predominantly mild winter climate. However, there are a few mountain ranges that contribute to snow accumulation. The Appalachian Mountains in northern Alabama, including the Cheaha, Dugger, and Talladega ranges, receive the most snowfall. These mountain ranges are crucial for the state's snowpack, as they provide runoff for several rivers and watersheds, including the Coosa, Tallapoosa, and Cahaba rivers. Winter climate characteristics in Alabama typically involve short-lived snow events followed by rapid melting due to the state's moderate temperatures. Interesting facts about snow science in Alabama are scarce, as snowfall is infrequent. Nevertheless, communities in the higher elevation areas of northern Alabama enjoy occasional snow-related activities. Overall, the limited snowpack in Alabama reflects the state's predominantly mild winter climate.