Physical and Chemical Data from the Nemo Expedition in the Ross Sea Aboard USCGC NORTHWIND (Ice Breaker) 2-23 February 1972.

The purpose of the USCGC Northwind's work was to measure the characteristics of the deep water in the western end of the Southeast Pacific Basin (71 degrees S to 75 degrees S and 140 degrees W to 170 degrees W) in order to determine whether bottom water formed in the Ross Sea flows into the Bas...

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Bibliographic Details
Other Authors: SCRIPPS INSTITUTION OF OCEANOGRAPHY LA JOLLA CALIF
Format: Text
Language:English
Published: 1974
Subjects:
Meteorology
Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*OCEANOGRAPHIC DATA
*ANTARCTIC REGIONS
*SOUTH PACIFIC OCEAN
TEMPERATURE
OCEAN SURFACE
CHEMICAL PROPERTIES
OCEAN BOTTOM SAMPLING
SEA WATER
MARINE METEOROLOGY
DEEP WATER
PATROL CRAFT
FLUID FLOW
SEA ICE
ICEBREAKERS
PLANKTON
TRITIUM
WAGB 282 Vessel
Ross Sea
Antarctic
Breaker
Pacific
Southeast Pacific Basin
Antarc*
Ice
permafrost
Sea ice
Online Access:http://www.dtic.mil/docs/citations/ADA000799
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA000799
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Summary:The purpose of the USCGC Northwind's work was to measure the characteristics of the deep water in the western end of the Southeast Pacific Basin (71 degrees S to 75 degrees S and 140 degrees W to 170 degrees W) in order to determine whether bottom water formed in the Ross Sea flows into the Basin. (Author)

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