A simplified three layer model is considered in order to examine the movements of deep mesoscale eddies such as the isolated Mediterranean eddies observed off the Bahamas. These anticyclonic eddies are found in the permanent thermocline more than 6000 km away from their parent water mass and are characterized by a lens-like cross section...
Mesoscale eddies (25 to 150 km diameter) are observed to occur along the crest of the Newfoundland R...
The total transport in the South Atlantic Ocean (Fig. 1) consists of an anticyclonic gyre that reach...
Author Posting. © American Meteorological Society, 2018. This article is posted here by permission ...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
The existence of a tongue of Mediterranean Water (MW) at the depths of 500–1500 m is a characteristi...
This is a report of the statistical behavior of neutrally buoyant SOFAR floats, drifting at 1500 m d...
As part of the POLYMODE experiment, three clusters (labeled A, B, C) of moored current meters and te...
Basin-wide geostrophic shear profiles have been computed for several latitudes in the eastern Atlant...
During 1977 two freely drifting buoys, originally in the Gulf Stream, looped over and in the lee of ...
Results from several numerical experiments based on one class of eddy-resolving gyre-scale models ha...
Above the deeper waters of the North Atlantic that have entered from the circumpolar flow, convectio...
A model is given that describes the local response of the upper ocean to an imposed surface wind str...
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deform...
Twenty neutrally buoyant SOFAR floats were used in the Mid-Ocean Dynamics Experiment (MODE) to study...
Time-averaged horizontal currents obtained from long-term moored instruments deployed in the western...
Mesoscale eddies (25 to 150 km diameter) are observed to occur along the crest of the Newfoundland R...
The total transport in the South Atlantic Ocean (Fig. 1) consists of an anticyclonic gyre that reach...
Author Posting. © American Meteorological Society, 2018. This article is posted here by permission ...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
The existence of a tongue of Mediterranean Water (MW) at the depths of 500–1500 m is a characteristi...
This is a report of the statistical behavior of neutrally buoyant SOFAR floats, drifting at 1500 m d...
As part of the POLYMODE experiment, three clusters (labeled A, B, C) of moored current meters and te...
Basin-wide geostrophic shear profiles have been computed for several latitudes in the eastern Atlant...
During 1977 two freely drifting buoys, originally in the Gulf Stream, looped over and in the lee of ...
Results from several numerical experiments based on one class of eddy-resolving gyre-scale models ha...
Above the deeper waters of the North Atlantic that have entered from the circumpolar flow, convectio...
A model is given that describes the local response of the upper ocean to an imposed surface wind str...
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deform...
Twenty neutrally buoyant SOFAR floats were used in the Mid-Ocean Dynamics Experiment (MODE) to study...
Time-averaged horizontal currents obtained from long-term moored instruments deployed in the western...
Mesoscale eddies (25 to 150 km diameter) are observed to occur along the crest of the Newfoundland R...
The total transport in the South Atlantic Ocean (Fig. 1) consists of an anticyclonic gyre that reach...
Author Posting. © American Meteorological Society, 2018. This article is posted here by permission ...