Add to ORKGA comparison is made between the geostrophic transport across selected latitudes in the North Atlantic Ocean and the theoretical transport as derived from the Sverdrup relationship. In the subtropical gyre these agree to within the error estimates. At 32°N and 24°N the interior geostrophic transports compare well with the measured values in the Florida Straits off Jacksonville
The warm, salty water influenced by the Mediterranean outflow can be observed at middepth throughout...
In order to produce a long-term mean circulation pattern for the western North Atlantic, geostrophic...
Many general circulation models predict a reduction in overturning strength in the 21st century as a...
Basin-wide geostrophic shear profiles have been computed for several latitudes in the eastern Atlant...
Quantitative agreement between geostrophic computations and direct measurements of current and trans...
Elementary Sverdrup balance is tested in the context of the time-average of a 16-year duration time-...
Three sets of recent data from the Southern Ocean, on mass transport through the Drake Passage (Whit...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deform...
Time-averaged horizontal currents obtained from long-term moored instruments deployed in the western...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
Godfrey\u27s (1989) (referred to below as G89) calculation of the global field of annual mean Depth-...
Using COADS data spanning 1947-1988, we describe the regional nature of the Atlantic Ocean wind-driv...
The warm, salty water influenced by the Mediterranean outflow can be observed at middepth throughout...
In order to produce a long-term mean circulation pattern for the western North Atlantic, geostrophic...
Many general circulation models predict a reduction in overturning strength in the 21st century as a...
Basin-wide geostrophic shear profiles have been computed for several latitudes in the eastern Atlant...
Quantitative agreement between geostrophic computations and direct measurements of current and trans...
Elementary Sverdrup balance is tested in the context of the time-average of a 16-year duration time-...
Three sets of recent data from the Southern Ocean, on mass transport through the Drake Passage (Whit...
Profiles of zonal velocity in the upper 500 m at the equator are computed from the differentiated fo...
A theory of the wind-driven ocean circulation is presented in which the key feature is strong deform...
Time-averaged horizontal currents obtained from long-term moored instruments deployed in the western...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
From historic meridional sections of the central equatorial Atlantic it is shown that the dynamic se...
Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the ...
Godfrey\u27s (1989) (referred to below as G89) calculation of the global field of annual mean Depth-...
Using COADS data spanning 1947-1988, we describe the regional nature of the Atlantic Ocean wind-driv...
The warm, salty water influenced by the Mediterranean outflow can be observed at middepth throughout...
In order to produce a long-term mean circulation pattern for the western North Atlantic, geostrophic...
Many general circulation models predict a reduction in overturning strength in the 21st century as a...