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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1979
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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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ARCTIC |
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32 |
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4 |
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