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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ftumich:oai:quod.lib.umich.edu:MIU01-102810985 2023-05-15T15:54:32+02:00 Tide and storm surge observations in the Chukchi Sea / Hunkins, Kenneth L. (Kenneth Leland), 1928- author. Lamont Geological Observatory, issuing body. Air Force Cambridge Research Laboratories (U.S.), issuing body. ncn http://hdl.handle.net/2027/nnc2.ark:/13960/t09w8zt79 eng eng http://hdl.handle.net/2027/nnc2.ark:/13960/t09w8zt79 Items in this record are available as Public Domain in the United States. View access and use profile at http://www.hathitrust.org/access_use#pd-us. Please see individual items for rights and use statements. PDM Tides Storm surges text Technical reports fast (OCoLC)fst01941336 ftumich 2022-08-28T13:40:19Z 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). "Contract AF 10 (604) 7442." "Project no. 7628, task no. 762805." "May 1963." "Prepared for Air Force Cambridge Research Laboratories, Office of Aerospace Research, Bedford, Massachusetts." Includes bibliographical references (pages 22-23). 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). Mode of access: Internet. Text Chukchi Chukchi Sea University of Michigan: Digital Collections Bedford ENVELOPE(-67.150,-67.150,-66.467,-66.467) Chukchi Sea |
institution |
Open Polar |
collection |
University of Michigan: Digital Collections |
op_collection_id |
ftumich |
language |
English |
topic |
Tides Storm surges |
spellingShingle |
Tides Storm surges Hunkins, Kenneth L. (Kenneth Leland), 1928- author. Lamont Geological Observatory, issuing body. Air Force Cambridge Research Laboratories (U.S.), issuing body. Tide and storm surge observations in the Chukchi Sea / |
topic_facet |
Tides Storm surges |
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). "Contract AF 10 (604) 7442." "Project no. 7628, task no. 762805." "May 1963." "Prepared for Air Force Cambridge Research Laboratories, Office of Aerospace Research, Bedford, Massachusetts." Includes bibliographical references (pages 22-23). 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). Mode of access: Internet. |
format |
Text |
author |
Hunkins, Kenneth L. (Kenneth Leland), 1928- author. Lamont Geological Observatory, issuing body. Air Force Cambridge Research Laboratories (U.S.), issuing body. |
author_facet |
Hunkins, Kenneth L. (Kenneth Leland), 1928- author. Lamont Geological Observatory, issuing body. Air Force Cambridge Research Laboratories (U.S.), issuing body. |
author_sort |
Hunkins, Kenneth L. (Kenneth Leland), 1928- author. |
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 / |
url |
http://hdl.handle.net/2027/nnc2.ark:/13960/t09w8zt79 |
long_lat |
ENVELOPE(-67.150,-67.150,-66.467,-66.467) |
geographic |
Bedford Chukchi Sea |
geographic_facet |
Bedford Chukchi Sea |
genre |
Chukchi Chukchi Sea |
genre_facet |
Chukchi Chukchi Sea |
op_relation |
http://hdl.handle.net/2027/nnc2.ark:/13960/t09w8zt79 |
op_rights |
Items in this record are available as Public Domain in the United States. View access and use profile at http://www.hathitrust.org/access_use#pd-us. Please see individual items for rights and use statements. |
op_rightsnorm |
PDM |
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1766389749985050624 |