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| My arctic research began as a doctoral candidate
at Queen's University under the supervision of Dr. Robert
Gilbert. While at Queen's I examined the physical, thermal, and geochemical
characteristics of ground ice near municipal water storage facilities on
Baffin Island in arctic Canada. My publications on this work use ice
wedge characteristics to reconstruct Holocene environmental change
as well as to evaluate the importance of subsurface cavities
in destabilizing ice-rich permafrost. Also, I have recently published two
papers in the 7th international permafrost conference proceedings. These
papers use cryostratigraphic and stable isotopic data to test hypotheses
of ground ice origin, as well as analyzing
ground temperature data to evaluate the extent to which reservoir construction
has modified ground thermal regimes.
Abstracts for these papers are given below. |
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Seasonal and mean annual ground temperature (MAGT) trends (1988-1991) are described for undisturbed, disturbed, and embankment sites to depths of 15 m at a large earthwork reservoir on southeastern Baffin Island. At sites away from the reservoir undisturbed and disturbed MAGT are similar, follow trends in air temperature, and indicate that climate has a greater influence on ground temperature than does thermal disturbance caused by land clearing. MAGT near the reservoir are warmest close to the high water line, and are cooler beneath a heated pumphouse, and under the crest of the embankment. Despite having the warmest absolute temperatures, water-side probes show the greatest and most rapid rates of cooling. This is attributed to the combination of climatically driven cooling trends and declining water levels in the reservoir. The validity of this hypothesis is confirmed by analytical models of temperature next to the water body. Reference: Hyatt, J. A. 1998. In: A. G. Lewkowicz and Allard, M. (editors), Proceedings, Seventh International Conference on Permafrost, Yellowknife, 23-27 June 1998, Universite Laval, Collection Nordicana no. 57, p. 479-486. |
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