OPERATION DEEP FREEZE 60. 1959-1960. OCEANOGRAPHIC SURVEY RESULTS

Results of oceanographic research during 19591960 are presented. Ships' tracks to, in, and from the Antarctic and locations of all oceanographic stations are given. In Eastern Balleny Basin, surface temperatures ranged from -0.44 to -1.58 C. Within the surface layer, temperature decreased to a...

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Other Authors: NAVAL OCEANOGRAPHIC OFFICE NSTL STATION MS
Format: Text
Language:English
Published: 1961
Subjects:
ICE
Online Access:http://www.dtic.mil/docs/citations/AD0260903
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0260903
id ftdtic:AD0260903
record_format openpolar
spelling ftdtic:AD0260903 2023-05-15T14:01:30+02:00 OPERATION DEEP FREEZE 60. 1959-1960. OCEANOGRAPHIC SURVEY RESULTS NAVAL OCEANOGRAPHIC OFFICE NSTL STATION MS 1961-06 text/html http://www.dtic.mil/docs/citations/AD0260903 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0260903 en eng http://www.dtic.mil/docs/citations/AD0260903 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS *HYDROGRAPHIC SURVEYING *OCEANOGRAPHY *POLAR REGIONS ICE OXYGEN SALINOMETERS SEDIMENTATION TEMPERATURE DEEP FREEZE OPERATION Text 1961 ftdtic 2016-02-21T11:04:44Z Results of oceanographic research during 19591960 are presented. Ships' tracks to, in, and from the Antarctic and locations of all oceanographic stations are given. In Eastern Balleny Basin, surface temperatures ranged from -0.44 to -1.58 C. Within the surface layer, temperature decreased to a depth of about 100 meters and then increased to a maximum of greater than 1.25 C, indicating the upper level of the Antarctic Circumpolar Water. Surface salinities were low (less than 34.00%). Values increased rapidly to 34.50% in the upper 200 meters with salinity maxima occurring between 600 and 1,200 meters depth. A west-east line of stations taken in McMurdo Sound is discussed. An extremely low temperature structure was noted, with temperatures from surface to bottom not exceeding 0.00 C throughout the water column. The effects of ice in the area were evident by low surface temperatures and salinities. Below the surface layer, temperatures decreased gradually to values as low as -1.93 C near the bottom of the deeper stations. Throughout the areas temperatures were less than 0 C, the degree of coldness indicating distance from the Ross Ice Shelf. (Author) Text Antarc* Antarctic Ice Shelf McMurdo Sound Ross Ice Shelf Defense Technical Information Center: DTIC Technical Reports database Antarctic Balleny Basin ENVELOPE(170.000,170.000,-67.000,-67.000) McMurdo Sound Ross Ice Shelf The Antarctic
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic *HYDROGRAPHIC SURVEYING
*OCEANOGRAPHY
*POLAR REGIONS
ICE
OXYGEN
SALINOMETERS
SEDIMENTATION
TEMPERATURE
DEEP FREEZE OPERATION
spellingShingle *HYDROGRAPHIC SURVEYING
*OCEANOGRAPHY
*POLAR REGIONS
ICE
OXYGEN
SALINOMETERS
SEDIMENTATION
TEMPERATURE
DEEP FREEZE OPERATION
OPERATION DEEP FREEZE 60. 1959-1960. OCEANOGRAPHIC SURVEY RESULTS
topic_facet *HYDROGRAPHIC SURVEYING
*OCEANOGRAPHY
*POLAR REGIONS
ICE
OXYGEN
SALINOMETERS
SEDIMENTATION
TEMPERATURE
DEEP FREEZE OPERATION
description Results of oceanographic research during 19591960 are presented. Ships' tracks to, in, and from the Antarctic and locations of all oceanographic stations are given. In Eastern Balleny Basin, surface temperatures ranged from -0.44 to -1.58 C. Within the surface layer, temperature decreased to a depth of about 100 meters and then increased to a maximum of greater than 1.25 C, indicating the upper level of the Antarctic Circumpolar Water. Surface salinities were low (less than 34.00%). Values increased rapidly to 34.50% in the upper 200 meters with salinity maxima occurring between 600 and 1,200 meters depth. A west-east line of stations taken in McMurdo Sound is discussed. An extremely low temperature structure was noted, with temperatures from surface to bottom not exceeding 0.00 C throughout the water column. The effects of ice in the area were evident by low surface temperatures and salinities. Below the surface layer, temperatures decreased gradually to values as low as -1.93 C near the bottom of the deeper stations. Throughout the areas temperatures were less than 0 C, the degree of coldness indicating distance from the Ross Ice Shelf. (Author)
author2 NAVAL OCEANOGRAPHIC OFFICE NSTL STATION MS
format Text
title OPERATION DEEP FREEZE 60. 1959-1960. OCEANOGRAPHIC SURVEY RESULTS
title_short OPERATION DEEP FREEZE 60. 1959-1960. OCEANOGRAPHIC SURVEY RESULTS
title_full OPERATION DEEP FREEZE 60. 1959-1960. OCEANOGRAPHIC SURVEY RESULTS
title_fullStr OPERATION DEEP FREEZE 60. 1959-1960. OCEANOGRAPHIC SURVEY RESULTS
title_full_unstemmed OPERATION DEEP FREEZE 60. 1959-1960. OCEANOGRAPHIC SURVEY RESULTS
title_sort operation deep freeze 60. 1959-1960. oceanographic survey results
publishDate 1961
url http://www.dtic.mil/docs/citations/AD0260903
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0260903
long_lat ENVELOPE(170.000,170.000,-67.000,-67.000)
geographic Antarctic
Balleny Basin
McMurdo Sound
Ross Ice Shelf
The Antarctic
geographic_facet Antarctic
Balleny Basin
McMurdo Sound
Ross Ice Shelf
The Antarctic
genre Antarc*
Antarctic
Ice Shelf
McMurdo Sound
Ross Ice Shelf
genre_facet Antarc*
Antarctic
Ice Shelf
McMurdo Sound
Ross Ice Shelf
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0260903
op_rights APPROVED FOR PUBLIC RELEASE
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