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troughAnatomical structure
The first long-term (250 d) current measurements from the southern trough of the CharlieGibbs Fracture Zone indicate persistent westward flow along the north wall and a steady eastward drift along the lower south wall. Net volume transport varies from westerly to easterly with a 2-3 month periodicity, but no seasonal cycle is evident. Overall, the separate westward and eastward transports are in balance...
A hydrographic section made in July 1977 from the research vessel KNORR revealed a large-scale merid...
As a sequel to Schmitz and Hogg (1978), nine-month moored observations of current and temperature fr...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
Historical temperature and salinity data from the Charlie-Gibbs Fracture Zone, including some 100 oc...
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...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
Spatially dense observations in consecutive years in a region within about 50 km of the continental ...
Mesoscale eddies (25 to 150 km diameter) are observed to occur along the crest of the Newfoundland R...
Basin-wide geostrophic shear profiles have been computed for several latitudes in the eastern Atlant...
When I returned to Woods Hole after serving in the Navy from 1943 to 1946, I worked as a technician ...
Observations of the hydrographic regime across the continental shelf and offshore to depths exceedin...
SOFAR float observations from 1300 m depth are used to describe a major feature of the large-scale, ...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
An array of near-bottom current meters was set on the continental rise and slope near Site D in the ...
A hydrographic section made in July 1977 from the research vessel KNORR revealed a large-scale merid...
As a sequel to Schmitz and Hogg (1978), nine-month moored observations of current and temperature fr...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
Historical temperature and salinity data from the Charlie-Gibbs Fracture Zone, including some 100 oc...
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...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
Spatially dense observations in consecutive years in a region within about 50 km of the continental ...
Mesoscale eddies (25 to 150 km diameter) are observed to occur along the crest of the Newfoundland R...
Basin-wide geostrophic shear profiles have been computed for several latitudes in the eastern Atlant...
When I returned to Woods Hole after serving in the Navy from 1943 to 1946, I worked as a technician ...
Observations of the hydrographic regime across the continental shelf and offshore to depths exceedin...
SOFAR float observations from 1300 m depth are used to describe a major feature of the large-scale, ...
From December 1965 to August 1967, the R/V CORIOLIS of the Centre O.R.S.T.O.M. of Nouméa made nine c...
An array of near-bottom current meters was set on the continental rise and slope near Site D in the ...
A hydrographic section made in July 1977 from the research vessel KNORR revealed a large-scale merid...
As a sequel to Schmitz and Hogg (1978), nine-month moored observations of current and temperature fr...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
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