Glacial Melt

Glacial melt refers to the process where glaciers—large masses of ice formed from compacted snow—are shrinking due to rising temperatures. As the climate warms, glaciers lose ice faster than new snow accumulates, leading to a gradual retreat. This melting contributes to rising sea levels, which can impact coastal communities and ecosystems. Additionally, glacial melt provides freshwater for rivers, lakes, and people, especially in regions that rely on this water during warmer months. Understanding glacial melt is crucial for assessing climate change and its effects on our planet's water resources and ecosystems.