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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Main Author: Hunkins, Kenneth L. Kenneth Leland, 1928-
Format: Text
Language:unknown
Published: Columbia University 1963
Subjects:
Online Access:https://dx.doi.org/10.7916/d8-92x5-8e62
https://academiccommons.columbia.edu/doi/10.7916/d8-92x5-8e62
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spelling ftdatacite:10.7916/d8-92x5-8e62 2024-09-09T19:36:26+00:00 Tide and storm surge observations in the Chukchi Sea ... Hunkins, Kenneth L. Kenneth Leland, 1928- 1963 https://dx.doi.org/10.7916/d8-92x5-8e62 https://academiccommons.columbia.edu/doi/10.7916/d8-92x5-8e62 unknown Columbia University Tides--Chukchi Sea Storm surges--Chukchi Sea article-journal Text ScholarlyArticle 1963 ftdatacite https://doi.org/10.7916/d8-92x5-8e62 2024-07-03T13:11:50Z 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). ... Text Chukchi Chukchi Sea DataCite Chukchi Sea
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language unknown
topic Tides--Chukchi Sea
Storm surges--Chukchi Sea
spellingShingle Tides--Chukchi Sea
Storm surges--Chukchi Sea
Hunkins, Kenneth L. Kenneth Leland, 1928-
Tide and storm surge observations in the Chukchi Sea ...
topic_facet Tides--Chukchi Sea
Storm surges--Chukchi Sea
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 Text
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 Columbia University
publishDate 1963
url https://dx.doi.org/10.7916/d8-92x5-8e62
https://academiccommons.columbia.edu/doi/10.7916/d8-92x5-8e62
geographic Chukchi Sea
geographic_facet Chukchi Sea
genre Chukchi
Chukchi Sea
genre_facet Chukchi
Chukchi Sea
op_doi https://doi.org/10.7916/d8-92x5-8e62
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