Snowmelt refers to the process of melting snow, which typically occurs in spring as temperatures rise. This melting contributes to the flow of rivers and streams, replenishing water supplies and supporting ecosystems. The timing and amount of snowmelt can vary based on factors like elevation, temperature, and local climate conditions. In many regions, especially mountainous areas, snowmelt is crucial for agriculture and water management. It provides essential irrigation for crops and helps maintain water levels in reservoirs. Understanding snowmelt patterns is important for predicting water availability and managing resources effectively, particularly in areas dependent on glaciers and snowpack.