HEAT FLOW DETERMINATIONS IN THE CANADIAN ARCTIC ARCHIPELAGO

Three heat flow determinations a were made in M'Clure Strait between Prince Patrick and Banks Islands in the northwestern part of the Arctic Archipelago of Canada. The three stations lie within 55 km of a point some 130 km SSW. of Mould Bay, Prince Patrick Island, and yield a weighted mean heat...

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Published in:Canadian Journal of Earth Sciences
Main Authors: Law, L. K., Paterson, W. S. B., Whitham, K.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1965
Subjects:
Online Access:http://dx.doi.org/10.1139/e65-006
http://www.nrcresearchpress.com/doi/pdf/10.1139/e65-006
id crcansciencepubl:10.1139/e65-006
record_format openpolar
spelling crcansciencepubl:10.1139/e65-006 2023-12-17T10:23:37+01:00 HEAT FLOW DETERMINATIONS IN THE CANADIAN ARCTIC ARCHIPELAGO Law, L. K. Paterson, W. S. B. Whitham, K. 1965 http://dx.doi.org/10.1139/e65-006 http://www.nrcresearchpress.com/doi/pdf/10.1139/e65-006 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 2, issue 2, page 59-71 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 1965 crcansciencepubl https://doi.org/10.1139/e65-006 2023-11-19T13:39:36Z Three heat flow determinations a were made in M'Clure Strait between Prince Patrick and Banks Islands in the northwestern part of the Arctic Archipelago of Canada. The three stations lie within 55 km of a point some 130 km SSW. of Mould Bay, Prince Patrick Island, and yield a weighted mean heat flow of 0.84 ± 0.09 μcal cm −2 s −1 , or 57% only of the worldwide continental average. The measurements were made from sea ice in water depths of some 430 m using a thermal probe and portable equipment carried in a fixed-wing aircraft.Instrumental limitations and errors are discussed, together with environmental factors. The uncertainties in interpreting this result as a truly subnormal equilibrium heat flow are outlined but it is concluded that the calculated systematic errors are unlikely to exceed 25%. Consequently in the absence of any known major perturbing effect, it must be concluded that the structure responsible for the suppression of vertical magnetic held variations at Mould Bay observatory does not extend 130 km to the south, is not produced by an anomalously high near-surface temperature, or is of late-Quaternary origin. Article in Journal/Newspaper Arctic Archipelago Arctic Canadian Arctic Archipelago M'Clure Strait Mould Bay Prince Patrick Island Sea ice Canadian Science Publishing (via Crossref) Arctic Canadian Arctic Archipelago Canada Mould Bay ENVELOPE(-119.436,-119.436,76.197,76.197) Prince Patrick Island ENVELOPE(-119.507,-119.507,76.751,76.751) M'Clure Strait ENVELOPE(-115.999,-115.999,74.498,74.498) Canadian Journal of Earth Sciences 2 2 59 71
institution Open Polar
collection Canadian Science Publishing (via Crossref)
op_collection_id crcansciencepubl
language English
topic General Earth and Planetary Sciences
spellingShingle General Earth and Planetary Sciences
Law, L. K.
Paterson, W. S. B.
Whitham, K.
HEAT FLOW DETERMINATIONS IN THE CANADIAN ARCTIC ARCHIPELAGO
topic_facet General Earth and Planetary Sciences
description Three heat flow determinations a were made in M'Clure Strait between Prince Patrick and Banks Islands in the northwestern part of the Arctic Archipelago of Canada. The three stations lie within 55 km of a point some 130 km SSW. of Mould Bay, Prince Patrick Island, and yield a weighted mean heat flow of 0.84 ± 0.09 μcal cm −2 s −1 , or 57% only of the worldwide continental average. The measurements were made from sea ice in water depths of some 430 m using a thermal probe and portable equipment carried in a fixed-wing aircraft.Instrumental limitations and errors are discussed, together with environmental factors. The uncertainties in interpreting this result as a truly subnormal equilibrium heat flow are outlined but it is concluded that the calculated systematic errors are unlikely to exceed 25%. Consequently in the absence of any known major perturbing effect, it must be concluded that the structure responsible for the suppression of vertical magnetic held variations at Mould Bay observatory does not extend 130 km to the south, is not produced by an anomalously high near-surface temperature, or is of late-Quaternary origin.
format Article in Journal/Newspaper
author Law, L. K.
Paterson, W. S. B.
Whitham, K.
author_facet Law, L. K.
Paterson, W. S. B.
Whitham, K.
author_sort Law, L. K.
title HEAT FLOW DETERMINATIONS IN THE CANADIAN ARCTIC ARCHIPELAGO
title_short HEAT FLOW DETERMINATIONS IN THE CANADIAN ARCTIC ARCHIPELAGO
title_full HEAT FLOW DETERMINATIONS IN THE CANADIAN ARCTIC ARCHIPELAGO
title_fullStr HEAT FLOW DETERMINATIONS IN THE CANADIAN ARCTIC ARCHIPELAGO
title_full_unstemmed HEAT FLOW DETERMINATIONS IN THE CANADIAN ARCTIC ARCHIPELAGO
title_sort heat flow determinations in the canadian arctic archipelago
publisher Canadian Science Publishing
publishDate 1965
url http://dx.doi.org/10.1139/e65-006
http://www.nrcresearchpress.com/doi/pdf/10.1139/e65-006
long_lat ENVELOPE(-119.436,-119.436,76.197,76.197)
ENVELOPE(-119.507,-119.507,76.751,76.751)
ENVELOPE(-115.999,-115.999,74.498,74.498)
geographic Arctic
Canadian Arctic Archipelago
Canada
Mould Bay
Prince Patrick Island
M'Clure Strait
geographic_facet Arctic
Canadian Arctic Archipelago
Canada
Mould Bay
Prince Patrick Island
M'Clure Strait
genre Arctic Archipelago
Arctic
Canadian Arctic Archipelago
M'Clure Strait
Mould Bay
Prince Patrick Island
Sea ice
genre_facet Arctic Archipelago
Arctic
Canadian Arctic Archipelago
M'Clure Strait
Mould Bay
Prince Patrick Island
Sea ice
op_source Canadian Journal of Earth Sciences
volume 2, issue 2, page 59-71
ISSN 0008-4077 1480-3313
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/e65-006
container_title Canadian Journal of Earth Sciences
container_volume 2
container_issue 2
container_start_page 59
op_container_end_page 71
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