STD observations in the southwest Atlantic from cruise 16, leg 9 of the R/V Conrad and cruise 7-75 of the Ara Islas Orcadas
Citable URI
https://hdl.handle.net/1912/10355DOI
10.1575/1912/10355Keyword
Salinity; Ocean temperatureAbstract
Continuous salinity-temperature-depth (STD) data from two cruises
in the South Atlantic are presented in both tabular and graphic form.
Thirty-seven of the stations were made during the R/V CONRAD cruise 16,
leg 9, March 29 to April 23, 1973 and 20 stations on the ARA ISLAS
ORCADAS cruise 7-75, October 30 to December 20, 1975.
Description
Includes Errata page dated 1 February 1980
Collections
Suggested Citation
Technical Report: Georgi, Daniel T., Amos, Anthony F., Draganovic, K. E., Raymer, Mary E., "STD observations in the southwest Atlantic from cruise 16, leg 9 of the R/V Conrad and cruise 7-75 of the Ara Islas Orcadas", 1979-08, DOI:10.1575/1912/10355, https://hdl.handle.net/1912/10355Related items
Showing items related by title, author, creator and subject.
-
The Subduction experiment : cruise report R/V Oceanus cruise number 250 legs 1 and 2 subduction 2 mooring deployment and recovery cruise, 25 January-26 February 1992
(Woods Hole Oceanographic Institution, 1993-03)Subduction is the mechanism by which water masses formed in the mixed layer and near the surface of the ocean find their way into the upper thermocline. The subduction process and its underlying mechanisms were studied ... -
The Marine light - mixed layer experiment cruise and data report, R/V Endeavor : cruise EN-224, mooring deployment, 27 April-1 May 1991, cruise EN-227, mooring recovery, 5-23 September 1991
(Woods Hole Oceanographic Institution, 1993-05)The Marine Light - Mixed Layer experiment took place in the sub-Arctic North Atlantic ocean, approximately 275 miles south of Reykjavik, Iceland. The field program included a central surface mooring to document the temporal ... -
The subduction experiment : cruise report R/V Knorr : cruise number 138 leg XV : subduction 3 mooring recovery cruise, 13-30 June 1993
(Woods Hole Oceanographic Institution, 1993-12)Subduction is the mechanism by which water masses formed in the mixed layer and near the surface of the ocean find their way into the upper thermocline. The subduction process and its underlying mechanisms were studied ...
