Chris Burn
Professor
Geography and Environmental Studies
Carleton University
Canada
Biography
Chris Burn is the supervisor of Carleton’s new Graduate Programs in Northern Studies. He held an NSERC Senior Northern Research Chair at the Department of Geography and Environmental Studies from 2002-12, throughout the program’s life. He came to Canada in 1981 as a Commonwealth Scholar, and completed both the M.A. (Geography, 1983) and Ph.D. (Geology, 1986) at Carleton. He then moved to U.B.C. as a Killam fellow, to study with J.Ross Mackay, the world authority in his field. In 1989 Chris was awarded an NSERC University Research Fellowship, which he brought back to Carleton in 1992. Chris is committed to long-term field investigations of frozen ground. His research is focused on the relations between climate and permafrost. He has been particularly interested in determining the response of ground temperatures and the active layer to climate warming as observed in the western Arctic since 1970. His program involves partnerships with several northern agencies, particularly AANDC, Yukon Parks, Parks Canada, the Village of Mayo, Yukon and Aurora Colleges, the City of Dawson, and the Departments of Transportation in Yukon and NWT. Dr Burn has been involved with the environmental and regulatory reviews of several northern projects, including the proposed Mackenzie Gas Project and, most recently, the Inuvik-Tuktoyaktuk Highway. His research program strives to provide explanations for the behaviour of permafrost terrain that are founded in field verification of physically based models. Projects completed and in progress at Herschel Island relate the present ground thermal regime to climate change over the past 120 years. Fieldwork there has also shown how temperatures inside an ice cellar at Pauline Cove allow comparison between convective and conductive heat transfer. Long-term observations at the Illisarvik drained lake field experiment build on Dr Mackay’s work, and have just given an uninterrupted 30-year record of active-layer development that may be the longest in North America. Ground temperatures collected at Illisarvik confirm the effect of regional warming in winter on summer thaw depth. In central and southern Yukon data collection is primarily concerned with the effect of changes in surface conditions on ground temperatures, especially following forest fire in Takhini River Valley, near Whitehorse, and after thaw slumping, near Mayo. Graduate student projects are woven into the general program that covers these themes. The work is supported by NSERC, PCSP, the Aurora Research Institute, Transport Canada, and AANDC. Northern agencies also provide critical assistance, especially the Village of Mayo, Herschel Island Qikiqtaruk Territorial Park, and Tuktut Nogait National Park. Since 1992, 20 Master’s and five PhD theses have been completed in the program, with one Ph.D. thesis and four M.Sc. projects underway.
Research Interest
Permafrost and ground ice Physical Geography of Yukon and Northwest Territories
Publications
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Burn, C.R. 1998. The response (1958 to 1997) of permafrost and near-surface ground temperatures to forest fire, Takhini River valley, southern Yukon Territory. Canadian Journal of Earth Sciences, 35(2): 184-199.
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Burn, C.R. 1997. Cryostratigraphy, paleogeography, and climate change during the early Holocene warm interval, western Arctic coast, Canada. Canadian Journal of Earth Sciences, 34(7): 912-925.
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Burn, C.R., and Smith, M.W. 1990. Development of thermokarst lakes during the Holocene at sites near Mayo, Yukon Territory. Permafrost and Periglacial Processes, 1(2): 161-176.
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Burn, C.R., and Smith, C.A.S. 1988. Observations of the “thermal offset†in mean annual ground temperature profiles at Mayo, Yukon Territory. Arctic, 41(2): 99‑104.