An early nineteenth century meteorological register from the eastern Canadian Arctic

Abstract Significant warming in the Arctic is anticipated for doubled-CO 2 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 Passa...

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Published in:Polar Record
Main Author: Kay, Paul A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1995
Subjects:
Online Access:https://doi.org/10.1017/s0032247400013887
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400013887
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author Kay, Paul A.
author_facet Kay, Paul A.
author_sort Kay, Paul A.
collection Cambridge University Press
container_issue 178
container_start_page 335
container_title Polar Record
container_volume 31
description Abstract Significant warming in the Arctic is anticipated for doubled-CO 2 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.
format Article in Journal/Newspaper
genre Arctic
Igloolik
Northwest passage
Northwest Territories
Polar Record
genre_facet Arctic
Igloolik
Northwest passage
Northwest Territories
Polar Record
geographic Arctic
Igloolik
Northwest Passage
Northwest Territories
Parry
geographic_facet Arctic
Igloolik
Northwest Passage
Northwest Territories
Parry
id crcambridgeupr:10.1017/s0032247400013887
institution Open Polar
language English
long_lat ENVELOPE(-81.800,-81.800,69.378,69.378)
ENVELOPE(-62.417,-62.417,-64.283,-64.283)
op_collection_id crcambridgeupr
op_container_end_page 342
op_doi https://doi.org/10.1017/s0032247400013887
op_rights https://www.cambridge.org/core/terms
op_source Polar Record
volume 31, issue 178, page 335-342
ISSN 0032-2474 1475-3057
publishDate 1995
publisher Cambridge University Press (CUP)
record_format openpolar
spelling crcambridgeupr:10.1017/s0032247400013887 2025-04-20T14:31:26+00:00 An early nineteenth century meteorological register from the eastern Canadian Arctic Kay, Paul A. 1995 https://doi.org/10.1017/s0032247400013887 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400013887 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Polar Record volume 31, issue 178, page 335-342 ISSN 0032-2474 1475-3057 journal-article 1995 crcambridgeupr https://doi.org/10.1017/s0032247400013887 2025-04-08T09:24:28Z Abstract Significant warming in the Arctic is anticipated for doubled-CO 2 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. Article in Journal/Newspaper Arctic Igloolik Northwest passage Northwest Territories Polar Record Cambridge University Press Arctic Igloolik ENVELOPE(-81.800,-81.800,69.378,69.378) Northwest Passage Northwest Territories Parry ENVELOPE(-62.417,-62.417,-64.283,-64.283) Polar Record 31 178 335 342
spellingShingle Kay, Paul A.
An early nineteenth century meteorological register from the eastern Canadian Arctic
title An early nineteenth century meteorological register from the eastern Canadian Arctic
title_full An early nineteenth century meteorological register from the eastern Canadian Arctic
title_fullStr An early nineteenth century meteorological register from the eastern Canadian Arctic
title_full_unstemmed An early nineteenth century meteorological register from the eastern Canadian Arctic
title_short An early nineteenth century meteorological register from the eastern Canadian Arctic
title_sort early nineteenth century meteorological register from the eastern canadian arctic
url https://doi.org/10.1017/s0032247400013887
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400013887