Permafrost carbon−climate feedback is sensitive to deep soil carbon decomposability but not deep soil nitrogen dynamics.

2015

Authors

• Charles Dunbar Koven
  • Lawrence Berkeley National Laboratory Earth and Environmental Sciences Area
• David M. Lawrence
  • National Center for Atmospheric Research Climate and Global Dynamics Division
• William J. Riley
  • Lawrence Berkeley National Laboratory Earth and Environmental Sciences Area

Editor

• Inez Y. Fung
  • University of California, Berkeley

Proceedings of the National Academy of Sciences of the United States of America volume 112 pages 3752–3757

DOI : 10.1073/pnas.1415123112

Provenance

• 1 report cites this article : usgcrp-ocpfy2017

This work is referenced by:

• Second State of the Carbon Cycle Report (SOCCR2): A Sustained Assessment Report (reference)
• chapter 12 (reference)
• Impacts, Risks, and Adaptation in the United States: The Fourth National Climate Assessment, Volume II (reference)
• chapter 2 (reference)
• finding 2.7 (reference)
• Climate Science Special Report: The Fourth National Climate Assessment: Volume I (reference)
• chapter 11 (reference)
• chapter 2 (reference)
• finding 11.2 (reference)

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