The hydrologic regime of Mackenzie River and connection of "no- closure' lakes to distributary channels in the Mackenzie Delta, Northwest Territories
Mackenzie Delta lakes have been classified by the seasonal duration of their connection to Mackenzie River. "No-closure' lakes are determined on the basis of minimum summer water level. Such lakes may become disconnected from the Mackenzie in autumn or winter, as water level falls or if th...
Published in: | Canadian Journal of Earth Sciences |
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Language: | English |
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1995
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Online Access: | https://ir.library.carleton.ca/pub/22843 https://doi.org/10.1139/e95-078 |
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ftcarletonunivir:oai:carleton.ca:22843 2023-05-15T17:09:29+02:00 The hydrologic regime of Mackenzie River and connection of "no- closure' lakes to distributary channels in the Mackenzie Delta, Northwest Territories Burn, C. (Christopher R.) 1995-01-01 https://ir.library.carleton.ca/pub/22843 https://doi.org/10.1139/e95-078 en eng https://ir.library.carleton.ca/pub/22843 doi:10.1139/e95-078 Canadian Journal of Earth Sciences vol. 32 no. 7, pp. 926-937 info:eu-repo/semantics/article 1995 ftcarletonunivir https://doi.org/10.1139/e95-078 2022-02-06T21:51:35Z Mackenzie Delta lakes have been classified by the seasonal duration of their connection to Mackenzie River. "No-closure' lakes are determined on the basis of minimum summer water level. Such lakes may become disconnected from the Mackenzie in autumn or winter, as water level falls or if the sills between lakes and distributary channels are frozen through and so sealed. Water level in the central delta rises continuously after late November, at first because discharge into the delta increases once the Mackenzie drainage basin has frozen over, and then as sea and channel ice thickens in the outer delta, impounding discharge. -from Author Article in Journal/Newspaper Mackenzie Delta Mackenzie river Northwest Territories Carleton University's Institutional Repository Northwest Territories Mackenzie River Mackenzie Delta ENVELOPE(-136.672,-136.672,68.833,68.833) Canadian Journal of Earth Sciences 32 7 926 937 |
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Open Polar |
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Carleton University's Institutional Repository |
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ftcarletonunivir |
language |
English |
description |
Mackenzie Delta lakes have been classified by the seasonal duration of their connection to Mackenzie River. "No-closure' lakes are determined on the basis of minimum summer water level. Such lakes may become disconnected from the Mackenzie in autumn or winter, as water level falls or if the sills between lakes and distributary channels are frozen through and so sealed. Water level in the central delta rises continuously after late November, at first because discharge into the delta increases once the Mackenzie drainage basin has frozen over, and then as sea and channel ice thickens in the outer delta, impounding discharge. -from Author |
format |
Article in Journal/Newspaper |
author |
Burn, C. (Christopher R.) |
spellingShingle |
Burn, C. (Christopher R.) The hydrologic regime of Mackenzie River and connection of "no- closure' lakes to distributary channels in the Mackenzie Delta, Northwest Territories |
author_facet |
Burn, C. (Christopher R.) |
author_sort |
Burn, C. (Christopher R.) |
title |
The hydrologic regime of Mackenzie River and connection of "no- closure' lakes to distributary channels in the Mackenzie Delta, Northwest Territories |
title_short |
The hydrologic regime of Mackenzie River and connection of "no- closure' lakes to distributary channels in the Mackenzie Delta, Northwest Territories |
title_full |
The hydrologic regime of Mackenzie River and connection of "no- closure' lakes to distributary channels in the Mackenzie Delta, Northwest Territories |
title_fullStr |
The hydrologic regime of Mackenzie River and connection of "no- closure' lakes to distributary channels in the Mackenzie Delta, Northwest Territories |
title_full_unstemmed |
The hydrologic regime of Mackenzie River and connection of "no- closure' lakes to distributary channels in the Mackenzie Delta, Northwest Territories |
title_sort |
hydrologic regime of mackenzie river and connection of "no- closure' lakes to distributary channels in the mackenzie delta, northwest territories |
publishDate |
1995 |
url |
https://ir.library.carleton.ca/pub/22843 https://doi.org/10.1139/e95-078 |
long_lat |
ENVELOPE(-136.672,-136.672,68.833,68.833) |
geographic |
Northwest Territories Mackenzie River Mackenzie Delta |
geographic_facet |
Northwest Territories Mackenzie River Mackenzie Delta |
genre |
Mackenzie Delta Mackenzie river Northwest Territories |
genre_facet |
Mackenzie Delta Mackenzie river Northwest Territories |
op_source |
Canadian Journal of Earth Sciences vol. 32 no. 7, pp. 926-937 |
op_relation |
https://ir.library.carleton.ca/pub/22843 doi:10.1139/e95-078 |
op_doi |
https://doi.org/10.1139/e95-078 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
32 |
container_issue |
7 |
container_start_page |
926 |
op_container_end_page |
937 |
_version_ |
1766065589814558720 |