Geophysical Data from Drifting Ice Station Fram III.

A scientific research camp was established on a drifting ice floe north of Spitsbergen on March 14, 1981, and occupied until May 13, 1981, while the floe drifted 361 km southwestward. Position of the camp was monitored with a satellite navigation system. Ocean depth was sounded continuously during t...

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Main Authors: Hunkins,Kenneth, Manley,T O, Tiemann,Werner, Jackson,Ruth
Other Authors: LAMONT-DOHERTY GEOLOGICAL OBSERVATORY PALISADES NY
Format: Text
Language:English
Published: 1981
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA109987
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA109987
id ftdtic:ADA109987
record_format openpolar
spelling ftdtic:ADA109987 2023-05-15T15:02:59+02:00 Geophysical Data from Drifting Ice Station Fram III. Hunkins,Kenneth Manley,T O Tiemann,Werner Jackson,Ruth LAMONT-DOHERTY GEOLOGICAL OBSERVATORY PALISADES NY 1981-12 text/html http://www.dtic.mil/docs/citations/ADA109987 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA109987 en eng http://www.dtic.mil/docs/citations/ADA109987 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography Geomagnetism Geodesy Snow Ice and Permafrost *ARCTIC OCEAN STATIONS POSITION(LOCATION) MOTION REFLECTION DEPTH DRIFT PROFILES SEISMIC WAVES TABLES(DATA) GRAVITY ROTATION OCEAN BOTTOM DEEP OCEANS SEA ICE FLOATING BODIES Ice floes Fram 3 ice station Magnetic declination Seismic reflection profiles Text 1981 ftdtic 2016-02-20T21:16:59Z A scientific research camp was established on a drifting ice floe north of Spitsbergen on March 14, 1981, and occupied until May 13, 1981, while the floe drifted 361 km southwestward. Position of the camp was monitored with a satellite navigation system. Ocean depth was sounded continuously during the drift as the camp crossed from the Farm Basin onto the Yermak Plateau. Rotation of the ice floe, magnetic declination and gravity were all measured frequently. Sub-bottom geological horizons were profiled with an air-gun and seismic reflection system. Data from all of these measurements are presented in the form of tables and profiles. Text Arctic Arctic Ocean Ice permafrost Sea ice Yermak plateau Spitsbergen Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean Yermak Plateau ENVELOPE(5.000,5.000,81.250,81.250)
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Physical and Dynamic Oceanography
Geomagnetism
Geodesy
Snow
Ice and Permafrost
*ARCTIC OCEAN
STATIONS
POSITION(LOCATION)
MOTION
REFLECTION
DEPTH
DRIFT
PROFILES
SEISMIC WAVES
TABLES(DATA)
GRAVITY
ROTATION
OCEAN BOTTOM
DEEP OCEANS
SEA ICE
FLOATING BODIES
Ice floes
Fram 3 ice station
Magnetic declination
Seismic reflection profiles
spellingShingle Physical and Dynamic Oceanography
Geomagnetism
Geodesy
Snow
Ice and Permafrost
*ARCTIC OCEAN
STATIONS
POSITION(LOCATION)
MOTION
REFLECTION
DEPTH
DRIFT
PROFILES
SEISMIC WAVES
TABLES(DATA)
GRAVITY
ROTATION
OCEAN BOTTOM
DEEP OCEANS
SEA ICE
FLOATING BODIES
Ice floes
Fram 3 ice station
Magnetic declination
Seismic reflection profiles
Hunkins,Kenneth
Manley,T O
Tiemann,Werner
Jackson,Ruth
Geophysical Data from Drifting Ice Station Fram III.
topic_facet Physical and Dynamic Oceanography
Geomagnetism
Geodesy
Snow
Ice and Permafrost
*ARCTIC OCEAN
STATIONS
POSITION(LOCATION)
MOTION
REFLECTION
DEPTH
DRIFT
PROFILES
SEISMIC WAVES
TABLES(DATA)
GRAVITY
ROTATION
OCEAN BOTTOM
DEEP OCEANS
SEA ICE
FLOATING BODIES
Ice floes
Fram 3 ice station
Magnetic declination
Seismic reflection profiles
description A scientific research camp was established on a drifting ice floe north of Spitsbergen on March 14, 1981, and occupied until May 13, 1981, while the floe drifted 361 km southwestward. Position of the camp was monitored with a satellite navigation system. Ocean depth was sounded continuously during the drift as the camp crossed from the Farm Basin onto the Yermak Plateau. Rotation of the ice floe, magnetic declination and gravity were all measured frequently. Sub-bottom geological horizons were profiled with an air-gun and seismic reflection system. Data from all of these measurements are presented in the form of tables and profiles.
author2 LAMONT-DOHERTY GEOLOGICAL OBSERVATORY PALISADES NY
format Text
author Hunkins,Kenneth
Manley,T O
Tiemann,Werner
Jackson,Ruth
author_facet Hunkins,Kenneth
Manley,T O
Tiemann,Werner
Jackson,Ruth
author_sort Hunkins,Kenneth
title Geophysical Data from Drifting Ice Station Fram III.
title_short Geophysical Data from Drifting Ice Station Fram III.
title_full Geophysical Data from Drifting Ice Station Fram III.
title_fullStr Geophysical Data from Drifting Ice Station Fram III.
title_full_unstemmed Geophysical Data from Drifting Ice Station Fram III.
title_sort geophysical data from drifting ice station fram iii.
publishDate 1981
url http://www.dtic.mil/docs/citations/ADA109987
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA109987
long_lat ENVELOPE(5.000,5.000,81.250,81.250)
geographic Arctic
Arctic Ocean
Yermak Plateau
geographic_facet Arctic
Arctic Ocean
Yermak Plateau
genre Arctic
Arctic Ocean
Ice
permafrost
Sea ice
Yermak plateau
Spitsbergen
genre_facet Arctic
Arctic Ocean
Ice
permafrost
Sea ice
Yermak plateau
Spitsbergen
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA109987
op_rights APPROVED FOR PUBLIC RELEASE
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