Effect of thermokarst lake margin expansion rate on sub-lake permafrost thaw in continuous permafrost
Andrea Creighton1, Andy Parsekian2, Michael Angelopoulos3, Benjamin M Jones4, Allen C Bondurant5, Paul Overduin6, Esther Babcock7, Melanie J Engram8 and Christopher D Arp5, (1)University of Wyoming, Laramie, WY, United States, (2)University of Wyoming, Department of Geology and Geophysics, Laramie, WY, United States, (3)Alfred Wegener Institute Helmholtz Center for Polar and Marine Research, Bremerhaven, Germany, (4)U.S. Geological Survey, Alaska Science Center, Anchorage, AK, United States, (5)University of Alaska Fairbanks, Water and Environmental Research Center, Fairbanks, United States, (6)Alfred Wegener Institute Helmholtz Center for Polar and Marine Research, Permafrost Research Section, Potsdam, Germany, (7)Logic Geophysics and Analytics LLC, Anchorage, United States, (8)University of Alaska Fairbanks, Fairbanks, AK, United States
