Rapid Permafrost Thaw Carbon Trajectories

Understanding how rapid Arctic permafrost thaw reshapes carbon emissions, climate feedbacks, and future climate trajectories.

Headwall of a thaw slump with helicopter, Peel Plateau, Canada. Credits: Carolina Voigt, AWI (2025).

About the PeTCaT Project

Permafrost soils in the Arctic store enormous amounts of organic carbon – more than currently found in the atmosphere. As the Arctic warms, frozen ground begins to thaw, potentially releasing large quantities of carbon dioxide (CO₂) and methane (CH₄) into the atmosphere and accelerating climate change.

While gradual permafrost thaw has been studied for decades, much less is known about rapid thaw processes such as thaw lakes, thaw slumps, erosion, and ground collapse. These abrupt landscape changes can expose deep, carbon-rich soils and trigger strong greenhouse gas emissions, yet they are still poorly represented in current Earth System Models.

PeTCaT brings together an international team of experts in permafrost science, greenhouse gas biogeochemistry, remote sensing, artificial intelligence, and climate modeling to better understand how rapid permafrost thaw affects the global carbon cycle and future climate trajectories.

Using field observations, satellite data, deep learning, laboratory experiments, and next-generation Earth System Models, PeTCaT will investigate where rapid thaw occurs, how much carbon becomes vulnerable, and how these emissions may alter the remaining global carbon budget for meeting climate targets.

The project will provide urgently needed scientific data and model-based insights for the research community, climate assessments, and decision-makers.


Knowledge Gaps and Challenges

More about gaps and challenges


Work Packages

Seven partner institutions from five countries are organized across seven work packages that together form PeTCaT. Learn more about our distributed research activities and the collaborators involved.

More about the work packages