B083:
Vulnerability of Permafrost Carbon to Climate Change

Submit an Abstract to this Session



Session ID#: 25556

Session Description:
Permafrost zone soils contain 1330-1580 Pg of organic carbon (C). Permafrost degradation can decrease ecosystem C storage by enhancing microbial activity and ecosystem respiration, but can also stimulate plant growth and lateral C flux, potentially increasing C stored in vegetation, soil, and sediment. This session invites papers that examine factors causing losses and gains in ecosystem C storage that relate to the question: What is the magnitude, timing, and form of C release from permafrost zone ecosystems to the atmosphere in a changing climate? Papers may address any aspect of this topic from molecular to global scales, using measurements or modeling to detect or forecast permafrost thaw and its influence on the C cycle and climate.
Primary Convener:  Edward Schuur, Northern Arizona University, Center for Ecosystem Science and Society, Flagstaff, AZ, United States
Convener:  Benjamin W Abbott, Brigham Young University, Provo, UT, United States

Cross-Listed:
  • C - Cryosphere
  • GC - Global Environmental Change
Index Terms:

Abstracts Submitted to this Session:

Kazuyuki Saito1, Hiroshi Ohno2, Tokuta Yokohata3, Go Iwahana4 and Hirokazu Machiya1, (1)JAMSTEC Japan Agency for Marine-Earth Science and Technology, Kanagawa, Japan, (2)Kitami Institute of Technology, Kitami, Japan, (3)NIES National Institute of Environmental Studies, Ibaraki, Japan, (4)University of Alaska Fairbanks, Fairbanks, AK, United States
Yonghong Yi, University of Montana, Numerical Terradynamic Simulation Group, College of Forestry & Conservation, Missoula, MT, United States, John S Kimball, The University of Montana, Numerical Terradynamic Simulation Group, Missoula, MT, United States, Mahta Moghaddam, The University of Michigan, Los Angeles, CA, United States, Richard H Chen, University of Southern California, Los Angeles, CA, United States, Rolf H Reichle, NASA GSFC, Greenbelt, MD, United States, Walter C Oechel, Open University, Milton Keynes, United Kingdom and Donatella Zona, San Diego State University, San Diego, CA, United States

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