Topological climate change with permafrost feedback

• Published in: Journal of Physics: Conference Series
• Main Authors: Kypke, Kolja L, Langford, William F, Nethercott, Nathaniel, Willms, Allan R
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: IOP Publishing 2021
• Subjects: Arctic; albedo; Climate change; Ice; permafrost
• Online Access: http://dx.doi.org/10.1088/1742-6596/1730/1/012090; https://iopscience.iop.org/article/10.1088/1742-6596/1730/1/012090; https://iopscience.iop.org/article/10.1088/1742-6596/1730/1/012090/pdf

Abstract Climate models predict that the climate of the Earth is warming and will continue to warm in coming centuries, if there is no mitigation. A recent energy balance model [Kypke et al., Nonlin. Process. Geophys. 27 (2020) 391–409] forecasts that, if the current increase of carbon dioxide in the atmosphere continues unabated, then in the next century the climate of the Earth will not only get warmer, but will transition abruptly via a bifurcation, to a warm equable climate unlike any climate seen on Earth since the Pliocene. This transition to a new climate state is a topological change . That model includes the effects of water vapour feedback and ice albedo feedback, as well as ocean and atmospheric heat transport. This paper adds to that model further amplification by permafrost feedback. That is, as the Arctic warms, permafrost will thaw, releasing large amounts of the greenhouse gases carbon dioxide and methane, which cause further warming. Since knowledge of permafrost stores and release rates is limited, a range of permafrost carbon release sensitivities ( Q 10 ) is considered. The model predicts that permafrost feedback accelerates the timing and increases the likelihood of a topological climate change in the Arctic, and reinforces the view that permafrost feedback should not be ignored in Anthropocene climate models.