Evaluates nitrogen release effects on future soil carbon losses, highlighting climate feedback importance.
fertilisation and increased nitrogen availability following thaw. However, the future vegetation carbon uptake due to increased nitrogen availability has only been quantified in a few studies and may be overestimated by our model. Therefore, its strength remains highly uncertain and care must be taken not to underestimate the permafrost carbon-climate feedback when designing climate change mitigation strategies.
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Gaillard et al. (2026) studied this question.
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