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Letter to the Editor

A comment on ‘Vulnerability of permafrost carbon to global warming. Part I: model description and role of heat generated by organic matter decomposition’ by D. V. Khvorostyanov et al. (2008)

Pages 577-578 | Received 25 Sep 2008, Accepted 19 Dec 2008, Published online: 18 Jan 2017

References

  • Alexeev, V., Nicolsky, D., Romanovsky, V. and Lawrence, D. 2007. An evaluation of deep soil configurations in the CLM3 for im-proved representation of permafrost, Geophys. Res. Lett. 34, L09502, 10.1029/2007GL029536.
  • Davidson, E. A. and Janssens, I. A. 2006. Temperature sensitivity of soil carbon decomposition and feedbacks to climate change. Nature 440, 165–173.
  • Delisle, G. 2007. Near-surface permafrost degradation: how se-vere during the 21st century?. Geophys. Res. Lett. 34, L09503, 10.1029/2007GL029323.
  • Khvorostyanov, D. V., Krinner, G., Ciais, P., Heimann, M. and Zimov, S. A. 2008a. Vulnerability of permafrost carbon to global warming. Part I: model description and role of heat generated by organic matter decomposition. Tellus 60B, 250–264.
  • Khvorostyanov, D. V., Ciais, P., Krinner, G., Zimov, S. A, Corradi, C. H. and co-authors. 2008b. Vulnerability of permafrost carbon to global warming. Part II: sensitivity of permafrost carbon stock to global warming. Tellus 60B, 265–275.
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