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An early nineteenth century meteorological register from the eastern Canadian Arctic

Published online by Cambridge University Press:  27 October 2009

Paul A. Kay
Paul A. Kay
Affiliation:
Department of Environment and Resource Studies, University of Waterloo, Waterloo, Ontario N2L 3G1, Canada
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Abstract

Significant warming in the Arctic is anticipated for doubled-CO2 scenarios, but temperatures in the eastern Canadian Arctic have not yet exhibited that trend in the last few decades. The spatial juxtaposition of the winter station in 1822–1823 of William Edward Parry's Northwest Passage expedition with the modern Igloolik Research Centre of the Science Institute of the Northwest Territories affords an opportunity for historical reconstruction and comparison. Parry's data are internally consistent. The association of colder temperatures with westerly and northerly winds, and wanner temperatures with easterly and southerly winds, is statistically significant. Temperatures are not exactly comparable between the two time periods because of differences in instrumentation, exposure, and frequency of readings. Nevertheless, in 1822–1823, November and December appear to have been cold and January to March mild compared to modern experience. Anomalously, winds were more frequently northerly (and less frequently westerly) in the latter months than in recent observations. Parry recorded two warm episodes in mid-winter, but, overall, it appears that the winter of 1822–1823 was not outside the range of modern experience.

Type
Articles
Information
Polar Record , Volume 31 , Issue 178 , July 1995 , pp. 335 - 342
Copyright
Copyright © Cambridge University Press 1995

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