ARCTIC Modification by an Ice Cover of the Tide in

ABSTRACT. The tide in Hudson Bay-James Bay is mainly semidiurnal. Admittance calculations between a reference signal and the water level observed at some gauging sites reveal that in the interior of Hudson Bay-James Bay the tide occurs earlier and its amplitude is reduced after the formation of an i...

Full description

Bibliographic Details
Main Authors: James Bay, Hudson Bay, Gabriel Godin
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1985
Subjects:
Arctic
Baie d'Hudson
Baie-d'Hudson
Hudson
Hudson Bay
Maurice
James Bay
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.534.7762
http://pubs.aina.ucalgary.ca/arctic/Arctic39-1-65.pdf
Description
Summary:ABSTRACT. The tide in Hudson Bay-James Bay is mainly semidiurnal. Admittance calculations between a reference signal and the water level observed at some gauging sites reveal that in the interior of Hudson Bay-James Bay the tide occurs earlier and its amplitude is reduced after the formation of an ice cover. Key words: tides, ice, modification of tides, Hudson Bay RkSUME. La mark dans les baies d'Hudson et James est surtout semi-diurne. Des calculs d'entree entre un signal de rtftrence et le niveau d'eau observe h quelques sites de mesure signalent qu'h l'inttrieur de ces baies, la marke se produit plus t6t et son amplitude est reduite avec la formation d'une couche de glace. Mots cles: marees, glace, modification des marks, baie d'Hudson Traduit pour le journal par Maurice Guibord.

Similar Items