Phase IFoundation
Background
Overview
Permafrost thawing is a direct and severe consequence of global warming, impacting global carbon cycles, infrastructure resilience, biodiversity, and indigenous populations, making it a crucial topic for Environment, Geography, and Disaster Management.
Permafrost is ground (soil, rock, or sediment) that remains frozen for two or more consecutive years, primarily found in the Arctic and high-altitude regions. Its thawing, driven by rising global temperatures, is a critical consequence of climate change with far-reaching environmental and socio-economic impacts.