Hudson Bay Ice Conditions

ABSTRACT. Monthly mean ice cover distributions for Hudson Bay have been derived, based upon an analysis of nine years of aerial reconnaissance and other data. Information is presented in map form, along with diseussian Of significant features. Ice break-up is seen to work southward from the western,...

Full description

Bibliographic Details
Main Authors: Eric W. Danielson, Jr. L
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.486.5069
http://pubs.aina.ucalgary.ca/arctic/arctic24-2-90.pdf
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.486.5069
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.486.5069 2023-05-15T14:19:36+02:00 Hudson Bay Ice Conditions Eric W. Danielson Jr. L The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.486.5069 http://pubs.aina.ucalgary.ca/arctic/arctic24-2-90.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.486.5069 http://pubs.aina.ucalgary.ca/arctic/arctic24-2-90.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.aina.ucalgary.ca/arctic/arctic24-2-90.pdf text ftciteseerx 2016-01-08T08:13:14Z ABSTRACT. Monthly mean ice cover distributions for Hudson Bay have been derived, based upon an analysis of nine years of aerial reconnaissance and other data. Information is presented in map form, along with diseussian Of significant features. Ice break-up is seen to work southward from the western, northern, and eastern edges of the Bay; the pattern seems to be a result of local topography, cur-rents, and persistent winds. Final melting occurs in August. Freeze-up commences in October, along the northwestern shore, and proceeds southeastward. The entire Bay is ice-covered by early January, except for persistent shore leads. RÉSUMÉ. Conditions de la glace dans la mer d’Hudson. A partir de l’analyse de neuf années de reconnaissances aériennes et d’autres données, on a pu déduire des moyennes mensuelles de distribution de la glace pour la mer d’Hudson. L‘informa-tion est présentte sous formes de cartes et de discussion des Cléments significatifs. On y voit que la débâcle progresse vers le sud à partir des marges ouest, nord et est de la mer; cette séquence semble être le résultat de la topographie locale, des courants et.des vents dominants. La fonte se termine en aofit. L’enge€wommence en octobre le long de la rive nord-ouest et progresse vers le sud-est. Sauf pow les chenaux côtiers persistants, la mer est entihrement gelée au début de janvier. Text Arctic Hudson Bay Unknown Hudson Hudson Bay Voit ENVELOPE(-65.530,-65.530,-66.658,-66.658)
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description ABSTRACT. Monthly mean ice cover distributions for Hudson Bay have been derived, based upon an analysis of nine years of aerial reconnaissance and other data. Information is presented in map form, along with diseussian Of significant features. Ice break-up is seen to work southward from the western, northern, and eastern edges of the Bay; the pattern seems to be a result of local topography, cur-rents, and persistent winds. Final melting occurs in August. Freeze-up commences in October, along the northwestern shore, and proceeds southeastward. The entire Bay is ice-covered by early January, except for persistent shore leads. RÉSUMÉ. Conditions de la glace dans la mer d’Hudson. A partir de l’analyse de neuf années de reconnaissances aériennes et d’autres données, on a pu déduire des moyennes mensuelles de distribution de la glace pour la mer d’Hudson. L‘informa-tion est présentte sous formes de cartes et de discussion des Cléments significatifs. On y voit que la débâcle progresse vers le sud à partir des marges ouest, nord et est de la mer; cette séquence semble être le résultat de la topographie locale, des courants et.des vents dominants. La fonte se termine en aofit. L’enge€wommence en octobre le long de la rive nord-ouest et progresse vers le sud-est. Sauf pow les chenaux côtiers persistants, la mer est entihrement gelée au début de janvier.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Eric W. Danielson
Jr. L
spellingShingle Eric W. Danielson
Jr. L
Hudson Bay Ice Conditions
author_facet Eric W. Danielson
Jr. L
author_sort Eric W. Danielson
title Hudson Bay Ice Conditions
title_short Hudson Bay Ice Conditions
title_full Hudson Bay Ice Conditions
title_fullStr Hudson Bay Ice Conditions
title_full_unstemmed Hudson Bay Ice Conditions
title_sort hudson bay ice conditions
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.486.5069
http://pubs.aina.ucalgary.ca/arctic/arctic24-2-90.pdf
long_lat ENVELOPE(-65.530,-65.530,-66.658,-66.658)
geographic Hudson
Hudson Bay
Voit
geographic_facet Hudson
Hudson Bay
Voit
genre Arctic
Hudson Bay
genre_facet Arctic
Hudson Bay
op_source http://pubs.aina.ucalgary.ca/arctic/arctic24-2-90.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.486.5069
http://pubs.aina.ucalgary.ca/arctic/arctic24-2-90.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
_version_ 1766291399876018176