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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1995
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Online Access: | http://dx.doi.org/10.1017/s0032247400013887 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400013887 |
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crcambridgeupr:10.1017/s0032247400013887 2024-03-03T08:41:27+00:00 An early nineteenth century meteorological register from the eastern Canadian Arctic Kay, Paul A. 1995 http://dx.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 General Earth and Planetary Sciences Ecology Geography, Planning and Development journal-article 1995 crcambridgeupr https://doi.org/10.1017/s0032247400013887 2024-02-08T08:26:05Z 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 Northwest Territories Northwest Passage Igloolik ENVELOPE(-81.800,-81.800,69.378,69.378) Parry ENVELOPE(-62.417,-62.417,-64.283,-64.283) Polar Record 31 178 335 342 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
General Earth and Planetary Sciences Ecology Geography, Planning and Development |
spellingShingle |
General Earth and Planetary Sciences Ecology Geography, Planning and Development Kay, Paul A. An early nineteenth century meteorological register from the eastern Canadian Arctic |
topic_facet |
General Earth and Planetary Sciences Ecology Geography, Planning and Development |
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 |
author |
Kay, Paul A. |
author_facet |
Kay, Paul A. |
author_sort |
Kay, Paul A. |
title |
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_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_sort |
early nineteenth century meteorological register from the eastern canadian arctic |
publisher |
Cambridge University Press (CUP) |
publishDate |
1995 |
url |
http://dx.doi.org/10.1017/s0032247400013887 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400013887 |
long_lat |
ENVELOPE(-81.800,-81.800,69.378,69.378) ENVELOPE(-62.417,-62.417,-64.283,-64.283) |
geographic |
Arctic Northwest Territories Northwest Passage Igloolik Parry |
geographic_facet |
Arctic Northwest Territories Northwest Passage Igloolik Parry |
genre |
Arctic Igloolik Northwest passage Northwest Territories Polar Record |
genre_facet |
Arctic Igloolik Northwest passage Northwest Territories Polar Record |
op_source |
Polar Record volume 31, issue 178, page 335-342 ISSN 0032-2474 1475-3057 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0032247400013887 |
container_title |
Polar Record |
container_volume |
31 |
container_issue |
178 |
container_start_page |
335 |
op_container_end_page |
342 |
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1792497191206518784 |