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Mesoscale Thermohaline, Sound Velocity and Baroclinic Flow Structure of the Pacific Subtropical Front During the Winter of 1980
Mesoscale Thermohaline Sound Velocity Baroclinic Flow
2009/2/9
The three-dimensional thermohaline. sound velocity and baroclinic flow structure of the. pacific sub-tropical front during January and February 1990 are discussed. The front is meander-like, with a wa...
On the Maintenance of the Subtropical Front and its Associated Countercurrent
Subtropical Front wind-driven circulation thermally driven flow
2009/1/20
In the North Pacific and Atlantic Oceans, the Subtropical Countercurrent is an eastward flow across the Subtropical Gyre at a latitude where a classical wind-driven circulation theory would predict a ...
The Three-Dimensional Circulation near the Eastern North pacific Subtropical Front
Three-Dimensional Circulation Subtropical Front Eastern North pacific
2009/1/19
The purpose of our study is to describe and compute the large-scale, three-dimensional circulation near the Subtropical Front in the eastern North Pacific along 31°N. This was accomplished through the...
Strong Current Events Related to a Subtropical Front in the Northeast Atlantic
Strong Current Events Northeast Atlantic Subtropical Front
2009/1/16
Long-term temperature and current-meter records from moorings in the northern Canary Basin display strong current events with time scales between one and three months and large vertical scales of seve...
Numerical Study of the Seasonal Variations of the Subtropical Front and the Subtropical Countercurrent
Numerical Study Seasonal Variations Subtropical Front Subtropical Countercurrent
2009/1/12
Response of the Subtropical Countercurrent and the Subtropical Front in the North Pacific Ocean to seasonally changing wind stress and thermal condition are examined using the same idealized numerical...
Turbulent Mixing at the Pacific Subtropical Front
Turbulent Mixing Pacific Subtropical Front
2009/1/6
Some advection of water across the North Pacific subtropical front occurs by the subduction of surface mixed layers from the north side of the front underneath surface waters on the south side. Cross-...
Remote Topographic Forcing of a Baroclinic Western Boundary Current: An Explanation for the Southland Current and the Pathway of the Subtropical Front East of New Zealand
Remote Topographic Forcing Baroclinic Western Boundary Current Southland Current New Zealand
2008/6/23
The Southland Current is a western boundary current adjacent to the South Island of New Zealand and flows along a segment of the Southern Hemisphere subtropical front (STF). The physical mechanisms th...