SEASONAL and ANNUAL VARIATIONS IN ICE COVER IN BAFFIN BAY and NORTHERN DAVIS STRAIT
The sea ice cover in Baffin Bay and northern Davis Strait is at a maximum in March and at a minimum in September. It depletes rapidly in July and August and grows rapidly during October and November. More annual variations were noticed during periods of ice cover depletion than during ice cover grow...
Published in: | The Canadian Geographer/Le Géographe canadien |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Wiley
1980
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Online Access: | http://dx.doi.org/10.1111/j.1541-0064.1980.tb00262.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1541-0064.1980.tb00262.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1541-0064.1980.tb00262.x |
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crwiley:10.1111/j.1541-0064.1980.tb00262.x 2024-10-13T14:06:11+00:00 SEASONAL and ANNUAL VARIATIONS IN ICE COVER IN BAFFIN BAY and NORTHERN DAVIS STRAIT DEY, B. 1980 http://dx.doi.org/10.1111/j.1541-0064.1980.tb00262.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1541-0064.1980.tb00262.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1541-0064.1980.tb00262.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Canadian Geographies / Géographies canadiennes volume 24, issue 4, page 368-384 ISSN 0008-3658 1541-0064 journal-article 1980 crwiley https://doi.org/10.1111/j.1541-0064.1980.tb00262.x 2024-09-17T04:50:11Z The sea ice cover in Baffin Bay and northern Davis Strait is at a maximum in March and at a minimum in September. It depletes rapidly in July and August and grows rapidly during October and November. More annual variations were noticed during periods of ice cover depletion than during ice cover growth periods. The paper presents a sea ice forecast model which is based on annual ice cover depletion and growth data 1968‐79 and which should be useful for planning navigation and drilling operations. Le couvert de glace dans la baie de Baffin et le nord du détroit de Davis atteint son maximum en mars et est réduit à son minimum en septembre. II régresse rapidement en juillet et en aoǔt et croǐt rapidement en octobre et en novembre. Plus de variations annuelles ont été observées pour les périodes de diminution du couvert de glace que pour les periodes de croissance de ce dernier. Cet article présente un modèle de prévision du couvert de glace lequel est basé sur les donnees relatives à la croissance et à la régression du couvert de glace pour la période 1968‐79. Ce modèle devrait ětre utile dans la planification de la navigation et des opérations de forage. Article in Journal/Newspaper Baffin Bay Baffin Bay Baffin Baie de Baffin Davis Strait Détroit de Davis Sea ice Wiley Online Library Baffin Bay Baie de Baffin ENVELOPE(-67.996,-67.996,74.001,74.001) Détroit de Davis ENVELOPE(-57.996,-57.996,65.001,65.001) The Canadian Geographer/Le Géographe canadien 24 4 368 384 |
institution |
Open Polar |
collection |
Wiley Online Library |
op_collection_id |
crwiley |
language |
English |
description |
The sea ice cover in Baffin Bay and northern Davis Strait is at a maximum in March and at a minimum in September. It depletes rapidly in July and August and grows rapidly during October and November. More annual variations were noticed during periods of ice cover depletion than during ice cover growth periods. The paper presents a sea ice forecast model which is based on annual ice cover depletion and growth data 1968‐79 and which should be useful for planning navigation and drilling operations. Le couvert de glace dans la baie de Baffin et le nord du détroit de Davis atteint son maximum en mars et est réduit à son minimum en septembre. II régresse rapidement en juillet et en aoǔt et croǐt rapidement en octobre et en novembre. Plus de variations annuelles ont été observées pour les périodes de diminution du couvert de glace que pour les periodes de croissance de ce dernier. Cet article présente un modèle de prévision du couvert de glace lequel est basé sur les donnees relatives à la croissance et à la régression du couvert de glace pour la période 1968‐79. Ce modèle devrait ětre utile dans la planification de la navigation et des opérations de forage. |
format |
Article in Journal/Newspaper |
author |
DEY, B. |
spellingShingle |
DEY, B. SEASONAL and ANNUAL VARIATIONS IN ICE COVER IN BAFFIN BAY and NORTHERN DAVIS STRAIT |
author_facet |
DEY, B. |
author_sort |
DEY, B. |
title |
SEASONAL and ANNUAL VARIATIONS IN ICE COVER IN BAFFIN BAY and NORTHERN DAVIS STRAIT |
title_short |
SEASONAL and ANNUAL VARIATIONS IN ICE COVER IN BAFFIN BAY and NORTHERN DAVIS STRAIT |
title_full |
SEASONAL and ANNUAL VARIATIONS IN ICE COVER IN BAFFIN BAY and NORTHERN DAVIS STRAIT |
title_fullStr |
SEASONAL and ANNUAL VARIATIONS IN ICE COVER IN BAFFIN BAY and NORTHERN DAVIS STRAIT |
title_full_unstemmed |
SEASONAL and ANNUAL VARIATIONS IN ICE COVER IN BAFFIN BAY and NORTHERN DAVIS STRAIT |
title_sort |
seasonal and annual variations in ice cover in baffin bay and northern davis strait |
publisher |
Wiley |
publishDate |
1980 |
url |
http://dx.doi.org/10.1111/j.1541-0064.1980.tb00262.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1541-0064.1980.tb00262.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1541-0064.1980.tb00262.x |
long_lat |
ENVELOPE(-67.996,-67.996,74.001,74.001) ENVELOPE(-57.996,-57.996,65.001,65.001) |
geographic |
Baffin Bay Baie de Baffin Détroit de Davis |
geographic_facet |
Baffin Bay Baie de Baffin Détroit de Davis |
genre |
Baffin Bay Baffin Bay Baffin Baie de Baffin Davis Strait Détroit de Davis Sea ice |
genre_facet |
Baffin Bay Baffin Bay Baffin Baie de Baffin Davis Strait Détroit de Davis Sea ice |
op_source |
Canadian Geographies / Géographies canadiennes volume 24, issue 4, page 368-384 ISSN 0008-3658 1541-0064 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1541-0064.1980.tb00262.x |
container_title |
The Canadian Geographer/Le Géographe canadien |
container_volume |
24 |
container_issue |
4 |
container_start_page |
368 |
op_container_end_page |
384 |
_version_ |
1812812243306283008 |