When I returned to Woods Hole after serving in the Navy from 1943 to 1946, I worked as a technician for F. C. Fuglister during his classic descriptions of Gulf Stream meanders and Gulf Stream ring formation. Our work resulted in a joint paper (Fuglister and Worthington, 1951) on a multiple ship survey of the Gulf Stream. It also resulted in my promotion to the scientific staff in September 1951...
In 1735 Walter Hoxton, on his chart of Chesapeake Bay, gave an early and accurate description of the...
The seasonal behavior of the Georges Bank Water mass is described from the context of the historic N...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
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...
During June 1966, nine velocity measurements were made with neutrally buoyant floats at a depth of a...
During 1977 two freely drifting buoys, originally in the Gulf Stream, looped over and in the lee of ...
The Eighteen Degree Water of the western North Atlantic is formed by deep convection in winter. The ...
Time-averaged horizontal currents obtained from long-term moored instruments deployed in the western...
Bimonthly hydrographic surveys were begun in May, 1978 to measure the spatial structure and temporal...
Worthington (1972a) advanced the hypothesis that winter cooling of the Gulf Stream south of New Engl...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
The region where the North Atlantic Current crosses the ocean around 50N is studied from a watermass...
This is a report of the statistical behavior of neutrally buoyant SOFAR floats, drifting at 1500 m d...
The first long-term (250 d) current measurements from the southern trough of the CharlieGibbs Fractu...
In 1735 Walter Hoxton, on his chart of Chesapeake Bay, gave an early and accurate description of the...
The seasonal behavior of the Georges Bank Water mass is described from the context of the historic N...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
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...
During June 1966, nine velocity measurements were made with neutrally buoyant floats at a depth of a...
During 1977 two freely drifting buoys, originally in the Gulf Stream, looped over and in the lee of ...
The Eighteen Degree Water of the western North Atlantic is formed by deep convection in winter. The ...
Time-averaged horizontal currents obtained from long-term moored instruments deployed in the western...
Bimonthly hydrographic surveys were begun in May, 1978 to measure the spatial structure and temporal...
Worthington (1972a) advanced the hypothesis that winter cooling of the Gulf Stream south of New Engl...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
The region where the North Atlantic Current crosses the ocean around 50N is studied from a watermass...
This is a report of the statistical behavior of neutrally buoyant SOFAR floats, drifting at 1500 m d...
The first long-term (250 d) current measurements from the southern trough of the CharlieGibbs Fractu...
In 1735 Walter Hoxton, on his chart of Chesapeake Bay, gave an early and accurate description of the...
The seasonal behavior of the Georges Bank Water mass is described from the context of the historic N...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...