Arctic Oceanographic Measurements from Drifting Ice Islands. (1). Gravity Observations. (2).

Investigations in hydroacoustics and marine geophysics were conducted from two drifting ice stations, T-3 and Arlis II, in the Arctic Ocean. Long range sound propagation experiments were made over a number of paths between ice stations and also with icebreakers. The signals from explosives are trans...

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Main Authors: Hunkins,Kenneth L., Talwani,Manik
Other Authors: LAMONT-DOHERTY GEOLOGICAL OBSERVATORY PALISADES N Y
Format: Text
Language:English
Published: 1971
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/AD0728803
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0728803
id ftdtic:AD0728803
record_format openpolar
spelling ftdtic:AD0728803 2023-05-15T14:44:37+02:00 Arctic Oceanographic Measurements from Drifting Ice Islands. (1). Gravity Observations. (2). Hunkins,Kenneth L. Talwani,Manik LAMONT-DOHERTY GEOLOGICAL OBSERVATORY PALISADES N Y 1971-04 text/html http://www.dtic.mil/docs/citations/AD0728803 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0728803 en eng http://www.dtic.mil/docs/citations/AD0728803 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Geology Geochemistry and Mineralogy Snow Ice and Permafrost Acoustics *MARINE GEOPHYSICS *ARCTIC REGIONS UNDERWATER SOUND SOUND TRANSMISSION ICEBREAKERS SEA ICE NAVIGATION MARINE GEOLOGY HYDROGRAPHIC SURVEYING OCEANOGRAPHIC SHIPS MAPS Text 1971 ftdtic 2016-02-21T21:27:38Z Investigations in hydroacoustics and marine geophysics were conducted from two drifting ice stations, T-3 and Arlis II, in the Arctic Ocean. Long range sound propagation experiments were made over a number of paths between ice stations and also with icebreakers. The signals from explosives are transmitted to great ranges in the Arctic surface SOFAR channel. The character of these signals is explained in principal by both ray and mode theory. Background noise is created by cracking and crushing of the ice cover. The sources and variability of the background noise are discussed. Geophysical investigations included navigation, ocean depth, gravity and magnetics. Marine geological investigations included bottom photography, nephelometry and coring. Improvement of accuracy of sea gravity measurements by consideration of the cross coupling and off leveling errors is discussed. The use of satellite navigation for increasing navigational accuracy and hence the accuracy of gravity measurements is described. (Author) Text Arctic Arctic Ocean Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Geology
Geochemistry and Mineralogy
Snow
Ice and Permafrost
Acoustics
*MARINE GEOPHYSICS
*ARCTIC REGIONS
UNDERWATER SOUND
SOUND TRANSMISSION
ICEBREAKERS
SEA ICE
NAVIGATION
MARINE GEOLOGY
HYDROGRAPHIC SURVEYING
OCEANOGRAPHIC SHIPS
MAPS
spellingShingle Geology
Geochemistry and Mineralogy
Snow
Ice and Permafrost
Acoustics
*MARINE GEOPHYSICS
*ARCTIC REGIONS
UNDERWATER SOUND
SOUND TRANSMISSION
ICEBREAKERS
SEA ICE
NAVIGATION
MARINE GEOLOGY
HYDROGRAPHIC SURVEYING
OCEANOGRAPHIC SHIPS
MAPS
Hunkins,Kenneth L.
Talwani,Manik
Arctic Oceanographic Measurements from Drifting Ice Islands. (1). Gravity Observations. (2).
topic_facet Geology
Geochemistry and Mineralogy
Snow
Ice and Permafrost
Acoustics
*MARINE GEOPHYSICS
*ARCTIC REGIONS
UNDERWATER SOUND
SOUND TRANSMISSION
ICEBREAKERS
SEA ICE
NAVIGATION
MARINE GEOLOGY
HYDROGRAPHIC SURVEYING
OCEANOGRAPHIC SHIPS
MAPS
description Investigations in hydroacoustics and marine geophysics were conducted from two drifting ice stations, T-3 and Arlis II, in the Arctic Ocean. Long range sound propagation experiments were made over a number of paths between ice stations and also with icebreakers. The signals from explosives are transmitted to great ranges in the Arctic surface SOFAR channel. The character of these signals is explained in principal by both ray and mode theory. Background noise is created by cracking and crushing of the ice cover. The sources and variability of the background noise are discussed. Geophysical investigations included navigation, ocean depth, gravity and magnetics. Marine geological investigations included bottom photography, nephelometry and coring. Improvement of accuracy of sea gravity measurements by consideration of the cross coupling and off leveling errors is discussed. The use of satellite navigation for increasing navigational accuracy and hence the accuracy of gravity measurements is described. (Author)
author2 LAMONT-DOHERTY GEOLOGICAL OBSERVATORY PALISADES N Y
format Text
author Hunkins,Kenneth L.
Talwani,Manik
author_facet Hunkins,Kenneth L.
Talwani,Manik
author_sort Hunkins,Kenneth L.
title Arctic Oceanographic Measurements from Drifting Ice Islands. (1). Gravity Observations. (2).
title_short Arctic Oceanographic Measurements from Drifting Ice Islands. (1). Gravity Observations. (2).
title_full Arctic Oceanographic Measurements from Drifting Ice Islands. (1). Gravity Observations. (2).
title_fullStr Arctic Oceanographic Measurements from Drifting Ice Islands. (1). Gravity Observations. (2).
title_full_unstemmed Arctic Oceanographic Measurements from Drifting Ice Islands. (1). Gravity Observations. (2).
title_sort arctic oceanographic measurements from drifting ice islands. (1). gravity observations. (2).
publishDate 1971
url http://www.dtic.mil/docs/citations/AD0728803
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0728803
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Ice
permafrost
Sea ice
genre_facet Arctic
Arctic Ocean
Ice
permafrost
Sea ice
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0728803
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766316097558020096