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...
Main Author: | |
---|---|
Other Authors: | |
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 |
_version_ |
1766317863300235264 |