Snowmelt Processes

Snowmelt processes refer to the gradual warming of snow and ice, causing them to change from solid to liquid water. This occurs primarily due to rising temperatures from sunshine, air temperature, and other environmental factors. When snow melts, the resulting water can flow into streams and rivers, replenishing water supplies. The rate of snowmelt affects water availability, agriculture, and ecosystems. It is influenced by local climate, terrain, and the depth of snow cover, and plays a crucial role in shaping seasonal water patterns in many regions.