Snowpack conditions in West Virginia vary across different mountain ranges, providing crucial water resources for the state. The primary mountain ranges that contribute to snowpack in West Virginia include the Allegheny Mountains, the Blue Ridge Mountains, and the Appalachian Mountains. These ranges are responsible for feeding several important rivers, such as the Potomac River, the Greenbrier River, and the Cheat River, which supply water to various watersheds across the state.

Winter climate characteristics in West Virginia typically involve cold temperatures and significant snowfall. The state experiences an average annual snowfall of 50 to 100 inches, with higher amounts in mountainous areas. Snowstorms are common, particularly during December through February.

West Virginia has a rich history in snow science and winter sports. It is home to popular ski resorts, such as Snowshoe Mountain and Canaan Valley Resort, attracting enthusiasts from across the region. Additionally, the state has been a pioneer in snow research, with organizations like the West Virginia Water Research Institute studying snowmelt processes and their impact on water resources.