Magnetic Observations at International Polar Year Stations in Canada

During the First International Polar Year (1982-83) magnetic observatories were established in northern Canada at Fort Rae, Fort Conger, and Clearwater Fiord. Repeat magnetic observations made during the centenary of the First Polar Year enable a determination of the secular variation at each of the...

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Published in:ARCTIC
Main Authors: Newitt, L.R., Dawson, E.
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1984
Subjects:
Rae
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65250
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/65250 2023-05-15T14:19:15+02:00 Magnetic Observations at International Polar Year Stations in Canada Newitt, L.R. Dawson, E. 1984-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65250 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65250/49164 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65250 ARCTIC; Vol. 37 No. 3 (1984): September: 195–320; 255-262 1923-1245 0004-0843 International Polar Year 1882-83 Geomagnetism History Research stations International Polar Year 1932-33 Clearwater Fiord region Nunavut Fort Conger Old Fort Rae N.W.T info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1984 ftunivcalgaryojs 2022-03-22T21:22:19Z During the First International Polar Year (1982-83) magnetic observatories were established in northern Canada at Fort Rae, Fort Conger, and Clearwater Fiord. Repeat magnetic observations made during the centenary of the First Polar Year enable a determination of the secular variation at each of these locations. During the last 100 years the declination has increased easterly by over 20 degrees at Fort Conger and at Clearwater Fiord; however, it has decreased by only 9 degrees at Fort Rae. The total intensity has decreased by over 1900 nT at Fort Rae, but at Clearwater Fiord and at Fort Conger the decrease has been about 1500 nT and 1000 nT respectively. This implies that the decrease in the non-dipole field evident over most of North America in recent times has not been as great in the high Arctic.Key words: Polar Year, Fort Conger, Fort Rae, Clearwater Fiord, Kingua Fiord, secular variation, magnetic field Mots clés: Année polaire, Fort Conger, Fort Rae, fjord Clearwater, fjord Kingua, variation séculaire, champ magnétique Article in Journal/Newspaper Arctic International Polar Year Nunavut University of Calgary Journal Hosting Canada Clearwater Fiord ENVELOPE(-67.447,-67.447,66.567,66.567) Fort Conger ENVELOPE(-64.742,-64.742,81.752,81.752) Nunavut Old Fort Rae ENVELOPE(-115.836,-115.836,62.650,62.650) Rae ENVELOPE(-116.053,-116.053,62.834,62.834) ARCTIC 37 3
institution Open Polar
collection University of Calgary Journal Hosting
op_collection_id ftunivcalgaryojs
language English
topic International Polar Year 1882-83
Geomagnetism
History
Research stations
International Polar Year 1932-33
Clearwater Fiord region
Nunavut
Fort Conger
Old Fort Rae
N.W.T
spellingShingle International Polar Year 1882-83
Geomagnetism
History
Research stations
International Polar Year 1932-33
Clearwater Fiord region
Nunavut
Fort Conger
Old Fort Rae
N.W.T
Newitt, L.R.
Dawson, E.
Magnetic Observations at International Polar Year Stations in Canada
topic_facet International Polar Year 1882-83
Geomagnetism
History
Research stations
International Polar Year 1932-33
Clearwater Fiord region
Nunavut
Fort Conger
Old Fort Rae
N.W.T
description During the First International Polar Year (1982-83) magnetic observatories were established in northern Canada at Fort Rae, Fort Conger, and Clearwater Fiord. Repeat magnetic observations made during the centenary of the First Polar Year enable a determination of the secular variation at each of these locations. During the last 100 years the declination has increased easterly by over 20 degrees at Fort Conger and at Clearwater Fiord; however, it has decreased by only 9 degrees at Fort Rae. The total intensity has decreased by over 1900 nT at Fort Rae, but at Clearwater Fiord and at Fort Conger the decrease has been about 1500 nT and 1000 nT respectively. This implies that the decrease in the non-dipole field evident over most of North America in recent times has not been as great in the high Arctic.Key words: Polar Year, Fort Conger, Fort Rae, Clearwater Fiord, Kingua Fiord, secular variation, magnetic field Mots clés: Année polaire, Fort Conger, Fort Rae, fjord Clearwater, fjord Kingua, variation séculaire, champ magnétique
format Article in Journal/Newspaper
author Newitt, L.R.
Dawson, E.
author_facet Newitt, L.R.
Dawson, E.
author_sort Newitt, L.R.
title Magnetic Observations at International Polar Year Stations in Canada
title_short Magnetic Observations at International Polar Year Stations in Canada
title_full Magnetic Observations at International Polar Year Stations in Canada
title_fullStr Magnetic Observations at International Polar Year Stations in Canada
title_full_unstemmed Magnetic Observations at International Polar Year Stations in Canada
title_sort magnetic observations at international polar year stations in canada
publisher The Arctic Institute of North America
publishDate 1984
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65250
long_lat ENVELOPE(-67.447,-67.447,66.567,66.567)
ENVELOPE(-64.742,-64.742,81.752,81.752)
ENVELOPE(-115.836,-115.836,62.650,62.650)
ENVELOPE(-116.053,-116.053,62.834,62.834)
geographic Canada
Clearwater Fiord
Fort Conger
Nunavut
Old Fort Rae
Rae
geographic_facet Canada
Clearwater Fiord
Fort Conger
Nunavut
Old Fort Rae
Rae
genre Arctic
International Polar Year
Nunavut
genre_facet Arctic
International Polar Year
Nunavut
op_source ARCTIC; Vol. 37 No. 3 (1984): September: 195–320; 255-262
1923-1245
0004-0843
op_relation https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65250/49164
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65250
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