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Integrated evaluation of the vulnerability to thermokarst disturbance and its implications for the regional carbon balance in boreal Alaska
Helene
Genet, Institute of Arctic Biology, hgenet@alaska.edu
Heather
Greaves, Institute of Arctic Biology, hegreaves@alaska.edu
(Presenter)
Mark
Jason
Lara, University of Alaska, Fairbanks, mjlara@alaska.edu
A.
David
McGuire, USGS, admcguire@alaska.edu
Bob
Bolton, University of Alaska, Fairbanks, bbolton@iarc.uaf.edu
Eugenie
Euskirchen, University of Alaska, Fairbanks, seeuskirchen@alaska.edu
Vladimir
Romanovsky, University of Alaska, Fairbanks, veromanovsky@alaska.edu
Our capacity to project future ecosystem trajectories in northern permafrost regions depends on our ability to characterize complex interactions between climatic and ecological processes at play in the soil, the vegetation, and the atmosphere. We present a study that uses remote sensing analyses, field observations, and data synthesis to inform models for the prediction of ecosystem responses to climate change in the boreal zone of Alaska.
Recent warming, altered precipitation and fire regimes are driving permafrost degradation, threatening to mobilize vast reservoirs of ancient carbon previously protected from decomposition. Although large scale, progressive, top-down permafrost thaw have been well studied and represented in high-latitude ecosystem models, the consequences of abrupt and local thermokarst disturbances (TK) are less well understood. To fill this gap, we conducted a detection analysis characterizing 60 years of land cover change in the Tanana Flats, a wetland complex subjected to TK disturbance in Interior Alaska, using aerial and satellite images. We observed a nonlinear loss of permafrost plateau forest associated with TK and driven by precipitation and forest fragmentation. The results of this analysis were integrated into the Alaska Thermokarst Model (ATM), a state-and-transition model that simulates land cover change associated with TK disturbance. Thermokarst-related land cover change was simulated from 2000 to 2100 across the Tanana Flats. By 2100, the model predicts a mean decrease of 26.5% (sd 7.2%) in permafrost plateau forests associated with an increase in TK fens and bogs.
Transitions from permafrost plateau forests to TK wetlands are accompanied with changes in physical and biogeochemical processes affecting ecosystem carbon balance. We evaluated the consequences of TK disturbances on the regional carbon balance by coupling outputs from the ATM and from a process-based biogeochemical model. We used long-term field observations of vegetation and soil physical and biogeochemical attributes to develop new parameterizations for TK wetlands and permafrost plateau forest land cover types. Preliminary simulations from 2000 to 2100 estimate that the conversion of permafrost plateau forest to young TK wetlands would result in a 28.0% (sd 3.5%) increase in Net Ecosystem Exchange.
Associated Project(s):
Poster Location ID: 64
Session Assigned: Permafrost and Hydrology
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