Tide and storm surge observations in the Chukchi Sea

Sea level heights were recorded with a tide gauge at Fletcher's Ice Island (T-3) while it was aground in the Chukchi Sea at 71:55 N, 160:20 W. Harmonic analyses were made for the tidal components. The tidal hour for M sub 2 is 9.11 at this location, in good agreement with the co-tidal chart of...

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Bibliographic Details
Main Author: Hunkins, Kenneth L. (Kenneth Leland), 1928-
Format: Report
Language:English
Published: Lamont Geological Laboratory, Columbia University 1963
Subjects:
Online Access:https://doi.org/10.7916/d8-92x5-8e62
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spelling ftcolumbiauniv:oai:academiccommons.columbia.edu:10.7916/d8-92x5-8e62 2023-05-15T15:54:30+02:00 Tide and storm surge observations in the Chukchi Sea Hunkins, Kenneth L. (Kenneth Leland), 1928- 1963 https://doi.org/10.7916/d8-92x5-8e62 English eng Lamont Geological Laboratory, Columbia University https://doi.org/10.7916/d8-92x5-8e62 Storm surges Tides Reports 1963 ftcolumbiauniv https://doi.org/10.7916/d8-92x5-8e62 2020-09-05T22:19:52Z Sea level heights were recorded with a tide gauge at Fletcher's Ice Island (T-3) while it was aground in the Chukchi Sea at 71:55 N, 160:20 W. Harmonic analyses were made for the tidal components. The tidal hour for M sub 2 is 9.11 at this location, in good agreement with the co-tidal chart of Sverdrup (1926). Storm surges observed at this location on the continental shelf have a range of about 40 cm. During relatively stationary atmospheric co-ions, the storm surge heights can be interpreted as due to the static water barometer effect. Dur ing conditions of moving atmospheric pressure systems, storm surge heights differ from those predicted by the water barometer effect. The combined application of Ekman's wind-driven current theory and Bernoulli's equation provides an explanation for these differences. (Author). Report Chukchi Chukchi Sea Columbia University: Academic Commons Chukchi Sea
institution Open Polar
collection Columbia University: Academic Commons
op_collection_id ftcolumbiauniv
language English
topic Storm surges
Tides
spellingShingle Storm surges
Tides
Hunkins, Kenneth L. (Kenneth Leland), 1928-
Tide and storm surge observations in the Chukchi Sea
topic_facet Storm surges
Tides
description Sea level heights were recorded with a tide gauge at Fletcher's Ice Island (T-3) while it was aground in the Chukchi Sea at 71:55 N, 160:20 W. Harmonic analyses were made for the tidal components. The tidal hour for M sub 2 is 9.11 at this location, in good agreement with the co-tidal chart of Sverdrup (1926). Storm surges observed at this location on the continental shelf have a range of about 40 cm. During relatively stationary atmospheric co-ions, the storm surge heights can be interpreted as due to the static water barometer effect. Dur ing conditions of moving atmospheric pressure systems, storm surge heights differ from those predicted by the water barometer effect. The combined application of Ekman's wind-driven current theory and Bernoulli's equation provides an explanation for these differences. (Author).
format Report
author Hunkins, Kenneth L. (Kenneth Leland), 1928-
author_facet Hunkins, Kenneth L. (Kenneth Leland), 1928-
author_sort Hunkins, Kenneth L. (Kenneth Leland), 1928-
title Tide and storm surge observations in the Chukchi Sea
title_short Tide and storm surge observations in the Chukchi Sea
title_full Tide and storm surge observations in the Chukchi Sea
title_fullStr Tide and storm surge observations in the Chukchi Sea
title_full_unstemmed Tide and storm surge observations in the Chukchi Sea
title_sort tide and storm surge observations in the chukchi sea
publisher Lamont Geological Laboratory, Columbia University
publishDate 1963
url https://doi.org/10.7916/d8-92x5-8e62
geographic Chukchi Sea
geographic_facet Chukchi Sea
genre Chukchi
Chukchi Sea
genre_facet Chukchi
Chukchi Sea
op_relation https://doi.org/10.7916/d8-92x5-8e62
op_doi https://doi.org/10.7916/d8-92x5-8e62
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