Winter Offshore/Onshore Wind Differences in Southeastern Hudson Bay, Canada

Acquisition of two 38-day wind data sets collected over a fast-ice shelf and at a nearby coastal weather station (Kuujjuarapik) in Hudson Bay allowed the calculation for the first time of an offshore/onshore wind speed ratio for an ice-covered environment. Mean wind over the ice was 29% higher than...

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Published in:ARCTIC
Main Author: Larouche, Pierre
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1990
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64645
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/64645 2023-05-15T14:19:13+02:00 Winter Offshore/Onshore Wind Differences in Southeastern Hudson Bay, Canada Larouche, Pierre 1990-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64645 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64645/48559 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64645 ARCTIC; Vol. 43 No. 1 (1990): March: 1–97; 55-59 1923-1245 0004-0843 Arctic Subarctic weather winds Hudson Bay comparison orographic effects offshore ice shelf Arctique subarctique météorologie vent baie d'Hudson comparaison effoertos graphiques banquise de glace info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1990 ftunivcalgaryojs 2022-03-22T21:21:48Z Acquisition of two 38-day wind data sets collected over a fast-ice shelf and at a nearby coastal weather station (Kuujjuarapik) in Hudson Bay allowed the calculation for the first time of an offshore/onshore wind speed ratio for an ice-covered environment. Mean wind over the ice was 29% higher than at the coast, compared to values of 65% for open ocean locations. This reflects the effect of the higher drag coefficient of the sea ice that more strongly attenuates the wind than does the sea surface. The data set also allowed the evaluation of the change in the wind field by local topography. Thus, a strong orographic effect was found in the SW quadrant, as winds of less than 5 m/s were deflected toward the SE and NW. Article in Journal/Newspaper Arctic Arctic Arctique* Baie d'Hudson banquise Hudson Bay Ice Shelf Kuujjuarapik Sea ice Subarctic subarctique* University of Calgary Journal Hosting Arctic Baie d'Hudson ENVELOPE(-78.666,-78.666,58.417,58.417) Baie-d'Hudson ENVELOPE(-74.999,-74.999,58.500,58.500) Canada Hudson Hudson Bay Kuujjuarapik ENVELOPE(-77.762,-77.762,55.276,55.276) ARCTIC 43 1
institution Open Polar
collection University of Calgary Journal Hosting
op_collection_id ftunivcalgaryojs
language English
topic Arctic
Subarctic
weather
winds
Hudson Bay
comparison
orographic effects
offshore
ice shelf
Arctique
subarctique
météorologie
vent
baie d'Hudson
comparaison
effoertos graphiques
banquise de glace
spellingShingle Arctic
Subarctic
weather
winds
Hudson Bay
comparison
orographic effects
offshore
ice shelf
Arctique
subarctique
météorologie
vent
baie d'Hudson
comparaison
effoertos graphiques
banquise de glace
Larouche, Pierre
Winter Offshore/Onshore Wind Differences in Southeastern Hudson Bay, Canada
topic_facet Arctic
Subarctic
weather
winds
Hudson Bay
comparison
orographic effects
offshore
ice shelf
Arctique
subarctique
météorologie
vent
baie d'Hudson
comparaison
effoertos graphiques
banquise de glace
description Acquisition of two 38-day wind data sets collected over a fast-ice shelf and at a nearby coastal weather station (Kuujjuarapik) in Hudson Bay allowed the calculation for the first time of an offshore/onshore wind speed ratio for an ice-covered environment. Mean wind over the ice was 29% higher than at the coast, compared to values of 65% for open ocean locations. This reflects the effect of the higher drag coefficient of the sea ice that more strongly attenuates the wind than does the sea surface. The data set also allowed the evaluation of the change in the wind field by local topography. Thus, a strong orographic effect was found in the SW quadrant, as winds of less than 5 m/s were deflected toward the SE and NW.
format Article in Journal/Newspaper
author Larouche, Pierre
author_facet Larouche, Pierre
author_sort Larouche, Pierre
title Winter Offshore/Onshore Wind Differences in Southeastern Hudson Bay, Canada
title_short Winter Offshore/Onshore Wind Differences in Southeastern Hudson Bay, Canada
title_full Winter Offshore/Onshore Wind Differences in Southeastern Hudson Bay, Canada
title_fullStr Winter Offshore/Onshore Wind Differences in Southeastern Hudson Bay, Canada
title_full_unstemmed Winter Offshore/Onshore Wind Differences in Southeastern Hudson Bay, Canada
title_sort winter offshore/onshore wind differences in southeastern hudson bay, canada
publisher The Arctic Institute of North America
publishDate 1990
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64645
long_lat ENVELOPE(-78.666,-78.666,58.417,58.417)
ENVELOPE(-74.999,-74.999,58.500,58.500)
ENVELOPE(-77.762,-77.762,55.276,55.276)
geographic Arctic
Baie d'Hudson
Baie-d'Hudson
Canada
Hudson
Hudson Bay
Kuujjuarapik
geographic_facet Arctic
Baie d'Hudson
Baie-d'Hudson
Canada
Hudson
Hudson Bay
Kuujjuarapik
genre Arctic
Arctic
Arctique*
Baie d'Hudson
banquise
Hudson Bay
Ice Shelf
Kuujjuarapik
Sea ice
Subarctic
subarctique*
genre_facet Arctic
Arctic
Arctique*
Baie d'Hudson
banquise
Hudson Bay
Ice Shelf
Kuujjuarapik
Sea ice
Subarctic
subarctique*
op_source ARCTIC; Vol. 43 No. 1 (1990): March: 1–97; 55-59
1923-1245
0004-0843
op_relation https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64645/48559
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/64645
container_title ARCTIC
container_volume 43
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