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Three-Dimensional Structure of Mesoscale Eddies in the Norwegian Coastal Current
Mesoscale Eddies Norwegian Coastal Current Three-Dimensional Structure
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2008/12/30
An eddy tracking experiment was carried out in the Norwegian Coastal Current during a 10-day field investigation period in February–March 1986. NOAA satellite infrared data were used in near real time...
Western Boundary Current Structure and Variability East of Abaco, Bahamas at 26.5°N
Deep Western Boundary Current Boundary Current Structure
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2008/12/27
During April 1987 to June 1988, a four-mooring, transport-resolving current meter array was deployed in a section extending 70 km eastward from Abaco, Bahamas, at 26.5°N. Mean currents in the upper la...
The Role of Finite Mixed-Layer Thickness in the Structure of the Ventilated Thermocline
Finite Mixed-Layer Thickness Ventilated Thermocline
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2008/12/24
A model of the ventilated thermocline consisting of three adiabatic layers surmounted by a mixed layer of finite thickness is presented. The mixed-layer depth density increase continuously northward, ...
Hydrographic Structure of the Convection Regime in the Gulf of Lions：Winter 1987
Hydrographic Structure northwestern Mediterranean Convection Regime
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2008/12/23
Deep winter convection in the northwestern Mediterranean (Gulf of Lions) and the subsequent formation of Mediterranean Deep Water were observed using advanced oceanographic instrumentation during a si...
Vertical Structure of the Seasonal Cycle in the Central Equatorial Atlantic Ocean：XBT Sections from 1980 to 1988
Vertical Structure Central Equatorial Atlantic Ocean Seasonal Cycle
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2008/12/23
A set of temperature profiles from expendable bathythermographs collected from 1980 to April 1988 along two ship routes transecting the equatorial Atlantic from 11°N to 11°S is analyzed to inter the v...
The Baroclinic Structure of the Abyssal Circulation
baroclinic model Abyssal Circulation
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2008/12/22
A simple baroclinic model of the abyssal ocean circulation is formulated in which the reversals of the meridional velocity with depth, and hence the layering of the abyss, is explained by the longitud...
Structure and Dynamics of the Rhodes Gyre System and Dynamical Interpolation for Estimates of the Mesoscale Variability
quasigeostrophic energy and vorticity analysis
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2008/12/22
A coastal quasigeostrophic (QG) methodology is extended in an exploration of the mesoscale variability of the Rhodes Gyre region of the Eastern Mediterranean Sea, given multiscale data taken as part o...
Effects of Friction on a Localized Structure in a Baroclinic Current
Baroclinic Current interfacial friction
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2008/12/19
In this paper, the effects of bottom and interfacial friction on localized baroclinic instability are discussed in the weakly nonlinear, long-wave limit. Using a quasigeostrophic two-layer model in wh...
Expected Structure of Extreme Waves in a Gaussian Sea. Part I：Theory and SWADE Buoy Measurements
Extreme Waves Gaussian Sea SWADE Buoy Measurements
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2008/12/18
This paper is concerned with the expected configuration in space and time surrounding extremely high crests in a random wave field, or, equivalently, the mean configuration averaged over realizations ...
Baroclinic Structure of the Abyssal Circulation and the Role of Meridional Topography
Baroclinic Structure Abyssal Circulation Meridional Topography
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2008/12/18
A simple linear model of the abyssal circulation is studied in which a north-south topographic slope influences the interior and boundary-layer flow. As in an earlier study, the reversals of the merid...
Structure of Intraseasonal Kelvin Waves in the Equatorial Pacific Ocean
Intraseasonal Kelvin Waves Equatorial Pacific Ocean
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2008/12/18
Previous studies have shown that intraseasonal Kelvin waves are a prominent mode of variability in the eastern and central equatorial Pacific. These waves appear to be remotely forced by wind variatio...
Structure of Velocity and Temperature in the Northeast Pacific as Measured with Lagrangian Drifters in Fall 1987
Northeast Pacific OCEAN STORMS Experiment Lagrangian surface drifters
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2008/12/18
In October 1987, 49 Lagrangian surface drifters (TRISTAR-II) were released in a 200-km × 200-km square area southeast of Ocean Station Papa as part of the OCEAN STORMS Experiment. The drifters measure...
Synthesizing the Gulf Stream Thermal Structure from XBT Data
Gulf Stream Thermal Structure XBT Data
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2008/12/17
Thirty-six XBT temperature profiles have been used in a parametric model introduced by Hendry to model the Gulf Stream's thermal structure at 65°W between 200 and 1200 dbar, with an rms residual error...
Observations of the Velocity and Vorticity Structure of Gulf Stream Meanders
acoustic Doppler current profiler Vorticity Structure Gulf Stream Meanders
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2008/12/17
In September–October 1988 and in April 1989 two 4-week cruises were organized to study the structure and dynamics of Gulf Stream meanders. The first one focused on an anticyclonic crest, and the secon...
Three-Dimensional Structure of the Wind-Driven Circulation in the Subtropical North Pacific
Three-Dimensional Structure Subtropical North Pacific Wind-Driven Circulation
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2008/12/16
The subduction rate is calculated for the North Pacific based on Levitus climatology data and Hellerman and Rosenstein wind stress data. Because the period of effective subduction is rather short, sub...