Effects of Storm Surges on the Beaufort Sea Coast, Northern Alaska

In 1970, a major storm surge caused by gale-force westerly winds inundated low-lying tundra plains and deltas as far as 5000 m inland and left a driftwood line as much as 3.4 m above normal sea level along the Beaufort Sea coast of Alaska. The height of the surge followed a predictable pattern and w...

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Published in:ARCTIC
Main Authors: Reimnitz, Erk, Maurer, Douglas K.
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 1979
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65683
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/65683 2023-05-15T14:19:18+02:00 Effects of Storm Surges on the Beaufort Sea Coast, Northern Alaska Reimnitz, Erk Maurer, Douglas K. 1979-01-01 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65683 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65683/49597 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65683 ARCTIC; Vol. 32 No. 4 (1979): December: 283–388; 329-344 1923-1245 0004-0843 Coast changes Erosion Shorelines Storm surges Alaska Northern Alaskan waters info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 1979 ftunivcalgaryojs 2022-03-22T21:22:45Z In 1970, a major storm surge caused by gale-force westerly winds inundated low-lying tundra plains and deltas as far as 5000 m inland and left a driftwood line as much as 3.4 m above normal sea level along the Beaufort Sea coast of Alaska. The height of the surge followed a predictable pattern and was highest along windward-facing shorelines. Coastal retreat and thermoerosion are greatly accelerated on such west-facing shores with eastward sediment transport opposite to normal littoral drift. Evidence suggests an approximate 100-year recurrence interval for similar surges, with potential for damaging the developing oil fields on the North Slope. Article in Journal/Newspaper Arctic Beaufort Sea north slope Tundra Alaska University of Calgary Journal Hosting ARCTIC 32 4
institution Open Polar
collection University of Calgary Journal Hosting
op_collection_id ftunivcalgaryojs
language English
topic Coast changes
Erosion
Shorelines
Storm surges
Alaska
Northern
Alaskan waters
spellingShingle Coast changes
Erosion
Shorelines
Storm surges
Alaska
Northern
Alaskan waters
Reimnitz, Erk
Maurer, Douglas K.
Effects of Storm Surges on the Beaufort Sea Coast, Northern Alaska
topic_facet Coast changes
Erosion
Shorelines
Storm surges
Alaska
Northern
Alaskan waters
description In 1970, a major storm surge caused by gale-force westerly winds inundated low-lying tundra plains and deltas as far as 5000 m inland and left a driftwood line as much as 3.4 m above normal sea level along the Beaufort Sea coast of Alaska. The height of the surge followed a predictable pattern and was highest along windward-facing shorelines. Coastal retreat and thermoerosion are greatly accelerated on such west-facing shores with eastward sediment transport opposite to normal littoral drift. Evidence suggests an approximate 100-year recurrence interval for similar surges, with potential for damaging the developing oil fields on the North Slope.
format Article in Journal/Newspaper
author Reimnitz, Erk
Maurer, Douglas K.
author_facet Reimnitz, Erk
Maurer, Douglas K.
author_sort Reimnitz, Erk
title Effects of Storm Surges on the Beaufort Sea Coast, Northern Alaska
title_short Effects of Storm Surges on the Beaufort Sea Coast, Northern Alaska
title_full Effects of Storm Surges on the Beaufort Sea Coast, Northern Alaska
title_fullStr Effects of Storm Surges on the Beaufort Sea Coast, Northern Alaska
title_full_unstemmed Effects of Storm Surges on the Beaufort Sea Coast, Northern Alaska
title_sort effects of storm surges on the beaufort sea coast, northern alaska
publisher The Arctic Institute of North America
publishDate 1979
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65683
genre Arctic
Beaufort Sea
north slope
Tundra
Alaska
genre_facet Arctic
Beaufort Sea
north slope
Tundra
Alaska
op_source ARCTIC; Vol. 32 No. 4 (1979): December: 283–388; 329-344
1923-1245
0004-0843
op_relation https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65683/49597
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/65683
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