Thaw-Depth

Thaw depth refers to the phenomenon where the ground, which is usually frozen in colder climates, begins to warm and soften during warmer months. This process occurs when temperatures rise above freezing, allowing the frozen soil and ice to melt. The thaw depth indicates how deep this melting reaches into the ground, which is important for understanding soil stability, plant growth, and infrastructure development. Farmers, builders, and environmental scientists monitor thaw depth to assess agricultural potential, construction feasibility, and ecological impacts in regions with seasonal freezing and thawing.