“…Potential feedbacks such as thawing permafrost (MacDougall and Friedlingstein, 2015;MacDougall et al, 2015;Burke et al, 2017;Gasser et al, 2018;Lowe and Bernie, 2018;MacDougall, 2021), peat land area and carbon evolution (Müller and Joos, 2021), ocean circulation changes due to ice melt from Greenland or Antarctica (Bronselaer et al, 2018;Lago and England, 2019;Li et al, 2023), feedbacks between warming, nitrous oxide and methane (Stocker et al, 2013;Battaglia and Joos, 2018;IPCC, 2021), and, on longer timescales than considered in this study, feedbacks associated with the potential melting and disintegration of polar ice sheets are currently missing from most ESMs. These feedbacks would potentially reduce the emission budget over time and potentially make negative emissions over long time periods necessary to maintain a stable temperature (Palazzo Corner et al, 2023).…”