Snowmelt

Snowmelt refers to the process of melting snow, typically occurring in spring as temperatures rise. As the sun warms the ground and air, snow absorbs heat, turning into water. This meltwater flows into rivers, lakes, and reservoirs, replenishing these water sources. Snowmelt is crucial for ecosystems and water supplies, especially in regions reliant on it for irrigation and drinking water. However, rapid snowmelt can lead to flooding, while insufficient melting can cause drought. The timing and amount of snowmelt are influenced by factors like temperature, precipitation, and snowpack levels.