Modification by an Ice Cover of the Tide in James Bay and Hudson Bay
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.K...
| Published in: | ARCTIC |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
The Arctic Institute of North America
1986
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| Subjects: | |
| Online Access: | https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65100 |
| Summary: | 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 Mots clés: Marées, glace, modification des marées, baie d'Hudson |
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