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Modeling soil thermal and carbon dynamics of a fire chronosequence in interior AlaskaAuthor(s): Q. Zhuang; A. D. McGuire; K. P. O'Neill; J. W. Harden; V. E. Romanovsky; J. Yarie
Source: Journal of Geophysical Research 108(D1):FFR 3-1 -- FFR 3-26
Publication Series: Scientific Journal (JRNL)
Station: North Central Research Station
PDF: Download Publication (3.29 MB)
DescriptionIn this study, the dynamics of soil thermal, hydrologic, and ecosystem processes were coupled to project how the carbon budgets of boreal forests will respond to changes in atmospheric CO2, climate, and fire disturbance. The ability of the model to simulate gross primary production and ecosystem respiration was verified for a mature black spruce ecosystem in Canada, the age-dependent pattern of the simulated vegetation carbon was verified with inventory data on aboveground growth of Alaskan black spruce forests, and the model was applied to a postfire chronosequence in interior Alaska. The comparison between the simulated soil temperature and field-based estimates during the growing season (May to September) of 1997 revealed that the model was able to accurately simulate monthly temperatures at 10 cm (R > 0.93) for control and burned stands of the fire chronosequence. Similarly, the simulated and field-based estimates of soil respiration for control and burned stands were correlated (R = 0.84 and 0.74 for control and burned stands, respectively). The simulated and observed decadal to century-scale dynamics of soil temperature and carbon dynamics, which are represented by mean monthly values of these variables during the growing season, were correlated among stands (R = 0.93 and 0.71 for soil temperature at 20- and 10-cm depths, R = 0.95 and 0.91 for soil respiration and soil carbon, respectively). Sensitivity analyses indicate that along with differences in fire and climate history a number of other factors influence the response of carbon dynamics to fire disturbance. These factors include nitrogen fixation, the growth of moss, changes in the depth of the organic layer, soil drainage, and fire severity.
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CitationZhuang, Q.; McGuire, A. D.; O''Neill, K. P.; Harden, J. W.; Romanovsky, V. E.; Yarie, J. 2003. Modeling soil thermal and carbon dynamics of a fire chronosequence in interior Alaska. Journal of Geophysical Research 108(D1):FFR 3-1 -- FFR 3-26
Keywordscarbon, fire, nitrogen, hydrology, permafrost
- The effects of fire on the thermal stability of permafrost in lowland and upland black spruce forests of interior Alaska in a changing climate
- Interactions between soil thermal and hydrological dynamics in the response of Alaska ecosystems to fire disturbance
- Recent acceleration of biomass burning and carbon losses in Alaskan forests and peatlands
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