Add to ORKGThe Eighteen Degree Water of the western North Atlantic is formed by deep convection in winter. The circulation and changing properties of Eighteen Degree Water are studied using hydrographic data from a long time series at the Panulirus station (32°10\u27N, 64°30\u27W) and from the Gulf Stream \u2760 experiment...
Mesoscale eddies (25 to 150 km diameter) are observed to occur along the crest of the Newfoundland R...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
During the summer of 1955, record high sea water temperatures were observed in harbors and coastal w...
A hydrographic section made in July 1977 from the research vessel KNORR revealed a large-scale merid...
When I returned to Woods Hole after serving in the Navy from 1943 to 1946, I worked as a technician ...
Hydrographic data at Ocean Station Echo (35N, 48W) form an almost continuous 6-year series ending in...
An array of 15 moorings with 33 current meters was deployed in the deep water across the Continental...
Bimonthly hydrographic surveys were begun in May, 1978 to measure the spatial structure and temporal...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
An example of long-term variability along 55W, perhaps interannual, for current and temperature dist...
Water mass interleaving observed over the N.W. African continental slope during Upwelling 75 has bee...
The results of a rapid survey of the Gulf of Mexico in the winter of 1962 are presented. Variations ...
Author Posting. © The Author(s), 2011. This is the author's version of the work. It is posted here ...
Microstructure profiles taken in February 2007 across the Gulf Stream (GS) measured the temporal and...
The annual variation in the structure and disposition of the principal water masses in the Gulf of M...
Mesoscale eddies (25 to 150 km diameter) are observed to occur along the crest of the Newfoundland R...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
During the summer of 1955, record high sea water temperatures were observed in harbors and coastal w...
A hydrographic section made in July 1977 from the research vessel KNORR revealed a large-scale merid...
When I returned to Woods Hole after serving in the Navy from 1943 to 1946, I worked as a technician ...
Hydrographic data at Ocean Station Echo (35N, 48W) form an almost continuous 6-year series ending in...
An array of 15 moorings with 33 current meters was deployed in the deep water across the Continental...
Bimonthly hydrographic surveys were begun in May, 1978 to measure the spatial structure and temporal...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
An example of long-term variability along 55W, perhaps interannual, for current and temperature dist...
Water mass interleaving observed over the N.W. African continental slope during Upwelling 75 has bee...
The results of a rapid survey of the Gulf of Mexico in the winter of 1962 are presented. Variations ...
Author Posting. © The Author(s), 2011. This is the author's version of the work. It is posted here ...
Microstructure profiles taken in February 2007 across the Gulf Stream (GS) measured the temporal and...
The annual variation in the structure and disposition of the principal water masses in the Gulf of M...
Mesoscale eddies (25 to 150 km diameter) are observed to occur along the crest of the Newfoundland R...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
During the summer of 1955, record high sea water temperatures were observed in harbors and coastal w...