The Southern Indian Lake Impoundment and Churchill River Diversion

The 242 000-km 2 Churchill River basin extends across the northern half of Alberta, Saskatchewan, and Manitoba. In 1976, hydraulic control structures were completed to divert 75% of the natural river flow of 958 m 3 ∙s −1 across the drainage divide separating the Churchill and Nelson river basins in...

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Published in:Canadian Journal of Fisheries and Aquatic Sciences
Main Authors: Newbury, R. W., McCullough, G. K., Hecky, R. E.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1984
Subjects:
Online Access:http://dx.doi.org/10.1139/f84-068
http://www.nrcresearchpress.com/doi/pdf/10.1139/f84-068
id crcansciencepubl:10.1139/f84-068
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spelling crcansciencepubl:10.1139/f84-068 2023-12-17T10:28:51+01:00 The Southern Indian Lake Impoundment and Churchill River Diversion Newbury, R. W. McCullough, G. K. Hecky, R. E. 1984 http://dx.doi.org/10.1139/f84-068 http://www.nrcresearchpress.com/doi/pdf/10.1139/f84-068 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Fisheries and Aquatic Sciences volume 41, issue 4, page 548-557 ISSN 0706-652X 1205-7533 Aquatic Science Ecology, Evolution, Behavior and Systematics journal-article 1984 crcansciencepubl https://doi.org/10.1139/f84-068 2023-11-19T13:39:23Z The 242 000-km 2 Churchill River basin extends across the northern half of Alberta, Saskatchewan, and Manitoba. In 1976, hydraulic control structures were completed to divert 75% of the natural river flow of 958 m 3 ∙s −1 across the drainage divide separating the Churchill and Nelson river basins in northern Manitoba. The diversion flows follow 300 km of tributary valleys southward to the Nelson River channel where a 30-yr, 10 000 MW hydroelectric scheme is being developed. The diversion was accomplished by damming the northern outlet of Southern Indian Lake, a 1977-km 2 riverine lake on the Churchill channel (latitude 57°N, longitude 99°W). The dam caused a 3-m impoundment above the historical lake levels, which flooded 414 km 2 of the backshore zone. Permafrost, or permanently frozen ground, is widespread in the uplands surrounding the lake. As bedrock occurred on only 14% of the postimpoundment shoreline, severe erosion of the frozen backshore deposits is now underway. A long period of instability is anticipated on lake shorelines and in river valleys affected by the altered hydraulic regime. Although the whole-lake water exchange time was increased by only 41% by the impoundment, the circulation patterns and exchange times in individual basins of the lake were changed dramatically when the Churchill waters were diverted at the southern end of the lake. The effects of the changing regimes on the aquatic habitats and fisheries of Southern Indian Lake have been investigated in pre- and post-impoundment studies undertaken by the Freshwater Institute of the Department of Fisheries and Oceans. Article in Journal/Newspaper Churchill Churchill River Nelson River permafrost Canadian Science Publishing (via Crossref) Indian Southern Indian Lake ENVELOPE(-98.500,-98.500,57.167,57.167) Canadian Journal of Fisheries and Aquatic Sciences 41 4 548 557
institution Open Polar
collection Canadian Science Publishing (via Crossref)
op_collection_id crcansciencepubl
language English
topic Aquatic Science
Ecology, Evolution, Behavior and Systematics
spellingShingle Aquatic Science
Ecology, Evolution, Behavior and Systematics
Newbury, R. W.
McCullough, G. K.
Hecky, R. E.
The Southern Indian Lake Impoundment and Churchill River Diversion
topic_facet Aquatic Science
Ecology, Evolution, Behavior and Systematics
description The 242 000-km 2 Churchill River basin extends across the northern half of Alberta, Saskatchewan, and Manitoba. In 1976, hydraulic control structures were completed to divert 75% of the natural river flow of 958 m 3 ∙s −1 across the drainage divide separating the Churchill and Nelson river basins in northern Manitoba. The diversion flows follow 300 km of tributary valleys southward to the Nelson River channel where a 30-yr, 10 000 MW hydroelectric scheme is being developed. The diversion was accomplished by damming the northern outlet of Southern Indian Lake, a 1977-km 2 riverine lake on the Churchill channel (latitude 57°N, longitude 99°W). The dam caused a 3-m impoundment above the historical lake levels, which flooded 414 km 2 of the backshore zone. Permafrost, or permanently frozen ground, is widespread in the uplands surrounding the lake. As bedrock occurred on only 14% of the postimpoundment shoreline, severe erosion of the frozen backshore deposits is now underway. A long period of instability is anticipated on lake shorelines and in river valleys affected by the altered hydraulic regime. Although the whole-lake water exchange time was increased by only 41% by the impoundment, the circulation patterns and exchange times in individual basins of the lake were changed dramatically when the Churchill waters were diverted at the southern end of the lake. The effects of the changing regimes on the aquatic habitats and fisheries of Southern Indian Lake have been investigated in pre- and post-impoundment studies undertaken by the Freshwater Institute of the Department of Fisheries and Oceans.
format Article in Journal/Newspaper
author Newbury, R. W.
McCullough, G. K.
Hecky, R. E.
author_facet Newbury, R. W.
McCullough, G. K.
Hecky, R. E.
author_sort Newbury, R. W.
title The Southern Indian Lake Impoundment and Churchill River Diversion
title_short The Southern Indian Lake Impoundment and Churchill River Diversion
title_full The Southern Indian Lake Impoundment and Churchill River Diversion
title_fullStr The Southern Indian Lake Impoundment and Churchill River Diversion
title_full_unstemmed The Southern Indian Lake Impoundment and Churchill River Diversion
title_sort southern indian lake impoundment and churchill river diversion
publisher Canadian Science Publishing
publishDate 1984
url http://dx.doi.org/10.1139/f84-068
http://www.nrcresearchpress.com/doi/pdf/10.1139/f84-068
long_lat ENVELOPE(-98.500,-98.500,57.167,57.167)
geographic Indian
Southern Indian Lake
geographic_facet Indian
Southern Indian Lake
genre Churchill
Churchill River
Nelson River
permafrost
genre_facet Churchill
Churchill River
Nelson River
permafrost
op_source Canadian Journal of Fisheries and Aquatic Sciences
volume 41, issue 4, page 548-557
ISSN 0706-652X 1205-7533
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/f84-068
container_title Canadian Journal of Fisheries and Aquatic Sciences
container_volume 41
container_issue 4
container_start_page 548
op_container_end_page 557
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