Siberian Permafrost

Siberian permafrost is a layer of permanently frozen soil found primarily in Siberia, Russia. It stays frozen year-round, affecting the local ecosystem, wildlife, and human activities. Permafrost can be several meters deep and holds significant amounts of carbon and methane, which are greenhouse gases. As global temperatures rise, this frozen ground is beginning to thaw, potentially releasing these gases into the atmosphere and contributing to climate change. Thawing can also damage infrastructure and alter landscapes, making the study of permafrost crucial for understanding environmental changes and their impacts.