Add to ORKGWorthington (1972a) advanced the hypothesis that winter cooling of the Gulf Stream south of New England is the cause of the Stream\u27s winter intensification. That loss of buoyancy should result in increased velocity and transport in an oceanic jet stream seems at first paradoxical...
The three-dimensional Princeton Ocean Model is used to examine the modification of the Gulf Stream a...
Mesoscale eddies (25 to 150 km diameter) are observed to occur along the crest of the Newfoundland R...
A hydrographic section made in July 1977 from the research vessel KNORR revealed a large-scale merid...
A simple model is used to explore a feedback mechanism which may be significant in the formation of ...
When I returned to Woods Hole after serving in the Navy from 1943 to 1946, I worked as a technician ...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deform...
Tlk zonal and temporal structure of the mean and low-frequency flow beneath the Gulf Stream at 55W i...
The three-dimensional Princeton Ocean Model is used to examine the modification of the Gulf Stream a...
A coastal geostrophic, baroclinic jet in the Gulf of Alaska is driven seasonally by fresh water disc...
Array measurements of current and temperature made for 15 months in the main thermodine of the Gulf ...
During 1977 two freely drifting buoys, originally in the Gulf Stream, looped over and in the lee of ...
Numerical solutions for a model of the World Ocean are analyzed to illustrate the important changes ...
Oceanic motions are partly driven by thermal forces associated with differential heating of the surf...
The three-dimensional Princeton Ocean Model is used to examine the modification of the Gulf Stream a...
The three-dimensional Princeton Ocean Model is used to examine the modification of the Gulf Stream a...
Mesoscale eddies (25 to 150 km diameter) are observed to occur along the crest of the Newfoundland R...
A hydrographic section made in July 1977 from the research vessel KNORR revealed a large-scale merid...
A simple model is used to explore a feedback mechanism which may be significant in the formation of ...
When I returned to Woods Hole after serving in the Navy from 1943 to 1946, I worked as a technician ...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deform...
Tlk zonal and temporal structure of the mean and low-frequency flow beneath the Gulf Stream at 55W i...
The three-dimensional Princeton Ocean Model is used to examine the modification of the Gulf Stream a...
A coastal geostrophic, baroclinic jet in the Gulf of Alaska is driven seasonally by fresh water disc...
Array measurements of current and temperature made for 15 months in the main thermodine of the Gulf ...
During 1977 two freely drifting buoys, originally in the Gulf Stream, looped over and in the lee of ...
Numerical solutions for a model of the World Ocean are analyzed to illustrate the important changes ...
Oceanic motions are partly driven by thermal forces associated with differential heating of the surf...
The three-dimensional Princeton Ocean Model is used to examine the modification of the Gulf Stream a...
The three-dimensional Princeton Ocean Model is used to examine the modification of the Gulf Stream a...
Mesoscale eddies (25 to 150 km diameter) are observed to occur along the crest of the Newfoundland R...
A hydrographic section made in July 1977 from the research vessel KNORR revealed a large-scale merid...