T7 Polar and Alpine Changes
Sunday, 22 October 2017
8:00 AM - 12:00 PM
Room 612
GROUNDWATER-PERMAFROST INTERACTIONS FOLLOWING FIRE: WATER AND ENERGY BALANCE EFFECTS
Paper number: T7-4
Program: Technical Sessions
Time: 8:45 AM – 9:00 AM
Authors
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Pierrick Lamontagne-HalleMcGill University, Montreal, QC
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Adrian V. RochaUniversity of Notre Dame, Notre Dame, IN
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Jeffrey McKenzieMcGill University Earth and Planetary Sciences, Montreal, QC
Abstract
We find that changes in the energy balance (increased soil temperature) are the dominant driver of post-fire permafrost thaw, but that hydrological properties of the subsurface (organic and mineral soil permeability) are the key control over the propagation of fire effects both vertically and laterally. Furthermore, we find that fire effects vary as a function of landscape position, with greater thaw in lowland settings due to advective heat transport from upland areas. These results indicate that the effects of fire are not necessarily confined only to burned regions, but can propagate laterally through groundwater flow to influence landscape-scale permafrost and hydrogeological processes. These results have implications for diverse high-latitude biogeochemical cycles, particularly in the context of future warming which is anticipated to both thaw permafrost and intensify fire regimes.
Geological Society of America Abstracts with Programs. Vol. 49, No. 6
doi: 10.1130/abs/2017AM-304224
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