B128
Vulnerability of Permafrost Carbon to Climate Change
Vulnerability of Permafrost Carbon to Climate Change
Session ID#: 81978
Session Description:
Permafrost carbon (C) remains one of the most important C cycle feedbacks to climate, with implications for global society. Permafrost region soils contain 1440-1600 billion tons of C; release of just a fraction of this pool as carbon dioxide and methane can accelerate climate change. Permafrost degradation can change ecosystem C storage by enhancing microbial activity and ecosystem respiration, but can also stimulate plant growth and increase C stored in vegetation and surface soil. This session invites papers that examine factors causing losses and gains in permafrost C that contribute to current observations and future projections of changing permafrost C through time. Papers may address any aspect of this topic from microbial communities to the global scale, using a range of field or laboratory measurements or modeling to detect and forecast permafrost thaw and the influence on the C cycle and future climate.
Co-Sponsor(s):
- WCRP: World Climate Research Programme -
Index Terms:
0428 Carbon cycling [BIOGEOSCIENCES]
0475 Permafrost, cryosphere, and high-latitude processes [BIOGEOSCIENCES]
0702 Permafrost [CRYOSPHERE]
1615 Biogeochemical cycles, processes, and modeling [GLOBAL CHANGE]
Primary Convener: Christina Schaedel, Northern Arizona University, Center for Ecosystem Science and Society (ECOSS), Flagstaff, AZ, United States
Convener: Elaine Pegoraro, Northern Arizona University, Flagstaff, AZ, United States
Primary Liaison: Christina Schaedel, Northern Arizona University, Center for Ecosystem Science and Society (ECOSS), Flagstaff, AZ, United States
See more of: Biogeosciences
