GEOPHYSICAL AND OCEANOGRAPHIC RESEARCH IN THE ARCTIC OCEAN

The use of stations on drifting pack ice for geophysical and oceanographic studies of the Arctic Ocean proved highly successful. The investigations by Lamont Geological Observatory from Drifting Stations Alpha, Bravo and Charlie provided new information about the environment of the Arctic Ocean. A p...

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Main Author: HUNKINS, KENNETH
Other Authors: LAMONT GEOLOGICAL OBSERVATORY PALISADES NY
Format: Text
Language:English
Published: 1960
Subjects:
Online Access:http://www.dtic.mil/docs/citations/AD0253807
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0253807
id ftdtic:AD0253807
record_format openpolar
spelling ftdtic:AD0253807 2023-05-15T14:46:40+02:00 GEOPHYSICAL AND OCEANOGRAPHIC RESEARCH IN THE ARCTIC OCEAN HUNKINS, KENNETH LAMONT GEOLOGICAL OBSERVATORY PALISADES NY 1960-11-15 text/html http://www.dtic.mil/docs/citations/AD0253807 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0253807 en eng http://www.dtic.mil/docs/citations/AD0253807 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS *ICE *OCEANOGRAPHIC DATA *OCEANOGRAPHY *SEISMIC WAVES *WEATHER STATIONS FLOATING BODIES GEOPHYSICS INSTRUMENTATION OCEAN BOTTOM OCEANS POLAR REGIONS PROPAGATION SEA WATER SOUND TRANSMISSION UNDERWATER SOUND WAVE PROPAGATION Text 1960 ftdtic 2016-02-21T11:03:32Z The use of stations on drifting pack ice for geophysical and oceanographic studies of the Arctic Ocean proved highly successful. The investigations by Lamont Geological Observatory from Drifting Stations Alpha, Bravo and Charlie provided new information about the environment of the Arctic Ocean. A prominent topographic feature, the Alpha Rise, was delineated and mapped from Station Alpha. The floor of the Arctic Ocean was observed directly for the first time in submarine bottom photographs. Unique deposits of gravel were found on the ocean floor and found to have been ice-rafted from a glacial shore area. Acoustic wave propagation in the ice revealed large seasonal changes in velocity. The Chukchi Rise was delineated in detail with fathograms produced by a precision depth recorder on Station Charlie. Long range deep-water underwater sound transmission was also observed from this station and the results interpreted in terms of normal mode theory. Finally, at Station Bravo, shallow-water underwater sound transmission was observed and found to agree with theory for normal modes propagating in an ice-water-sediment system. (Author) Text Arctic Arctic Ocean Chukchi Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean Chukchi Rise ENVELOPE(-165.000,-165.000,78.000,78.000) Water Sound ENVELOPE(-97.919,-97.919,76.535,76.535)
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic *ICE
*OCEANOGRAPHIC DATA
*OCEANOGRAPHY
*SEISMIC WAVES
*WEATHER STATIONS
FLOATING BODIES
GEOPHYSICS
INSTRUMENTATION
OCEAN BOTTOM
OCEANS
POLAR REGIONS
PROPAGATION
SEA WATER
SOUND TRANSMISSION
UNDERWATER SOUND
WAVE PROPAGATION
spellingShingle *ICE
*OCEANOGRAPHIC DATA
*OCEANOGRAPHY
*SEISMIC WAVES
*WEATHER STATIONS
FLOATING BODIES
GEOPHYSICS
INSTRUMENTATION
OCEAN BOTTOM
OCEANS
POLAR REGIONS
PROPAGATION
SEA WATER
SOUND TRANSMISSION
UNDERWATER SOUND
WAVE PROPAGATION
HUNKINS, KENNETH
GEOPHYSICAL AND OCEANOGRAPHIC RESEARCH IN THE ARCTIC OCEAN
topic_facet *ICE
*OCEANOGRAPHIC DATA
*OCEANOGRAPHY
*SEISMIC WAVES
*WEATHER STATIONS
FLOATING BODIES
GEOPHYSICS
INSTRUMENTATION
OCEAN BOTTOM
OCEANS
POLAR REGIONS
PROPAGATION
SEA WATER
SOUND TRANSMISSION
UNDERWATER SOUND
WAVE PROPAGATION
description The use of stations on drifting pack ice for geophysical and oceanographic studies of the Arctic Ocean proved highly successful. The investigations by Lamont Geological Observatory from Drifting Stations Alpha, Bravo and Charlie provided new information about the environment of the Arctic Ocean. A prominent topographic feature, the Alpha Rise, was delineated and mapped from Station Alpha. The floor of the Arctic Ocean was observed directly for the first time in submarine bottom photographs. Unique deposits of gravel were found on the ocean floor and found to have been ice-rafted from a glacial shore area. Acoustic wave propagation in the ice revealed large seasonal changes in velocity. The Chukchi Rise was delineated in detail with fathograms produced by a precision depth recorder on Station Charlie. Long range deep-water underwater sound transmission was also observed from this station and the results interpreted in terms of normal mode theory. Finally, at Station Bravo, shallow-water underwater sound transmission was observed and found to agree with theory for normal modes propagating in an ice-water-sediment system. (Author)
author2 LAMONT GEOLOGICAL OBSERVATORY PALISADES NY
format Text
author HUNKINS, KENNETH
author_facet HUNKINS, KENNETH
author_sort HUNKINS, KENNETH
title GEOPHYSICAL AND OCEANOGRAPHIC RESEARCH IN THE ARCTIC OCEAN
title_short GEOPHYSICAL AND OCEANOGRAPHIC RESEARCH IN THE ARCTIC OCEAN
title_full GEOPHYSICAL AND OCEANOGRAPHIC RESEARCH IN THE ARCTIC OCEAN
title_fullStr GEOPHYSICAL AND OCEANOGRAPHIC RESEARCH IN THE ARCTIC OCEAN
title_full_unstemmed GEOPHYSICAL AND OCEANOGRAPHIC RESEARCH IN THE ARCTIC OCEAN
title_sort geophysical and oceanographic research in the arctic ocean
publishDate 1960
url http://www.dtic.mil/docs/citations/AD0253807
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0253807
long_lat ENVELOPE(-165.000,-165.000,78.000,78.000)
ENVELOPE(-97.919,-97.919,76.535,76.535)
geographic Arctic
Arctic Ocean
Chukchi Rise
Water Sound
geographic_facet Arctic
Arctic Ocean
Chukchi Rise
Water Sound
genre Arctic
Arctic Ocean
Chukchi
genre_facet Arctic
Arctic Ocean
Chukchi
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0253807
op_rights APPROVED FOR PUBLIC RELEASE
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