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The Relationship Between Stability and Source Waters for a Section in the Northeast Atlantic
Stability Source Waters Northeast Atlantic
2009/4/2
The mean density structure in the Northeast Atlantic is described in terms of the stability frequency. Some dynamic considerations are given to account for the observed distribution and to indicate th...
The Relationship of the Curl of the Local Wind Stress to the Circulation of the Cayman Sea and the Gulf of Mexico
Local Wind Stress Gulf of Mexico Cayman Sea
2009/2/23
The curl of the annual mean wind stress is proposed as the forcing mechanism for the anticyclonic gyre observed in the Cayman Sea. A simple wind-driven model is presented to illustrate how a steady-st...
The Relationship of Tidal and Low-Frequency Currents on the North Slope of Georges Bank
Tidal Low-Frequency Currents North Slope of Georges Bank
2009/2/18
Measured currents at the steeply sloping north edge of Georges Bank show an unusually strong correlation between tidal and lower frequency components. The dominant current constituents are the rotary ...
Model for the Thickness and Salinity of the Upper Layer in the Arctic Ocean and the Relationship between the Ice Thickness and Some External Parameters
Upper Layer Arctic Ocean Ice Thickness External Parameters
2009/2/10
This paper presents a dynamical model for the salinity and thickness of the upper layer in the Arctic. The parameters are the river runoff to the Arctic, the buoyancy supply through the Bering Strait,...
Form of the Temperature-Salinity Relationship in the Central Water：Evidence for Double-Diffusive Mixing
Temperature-Salinity Double-Diffusive Mixing Central Water
2009/2/10
Ingham (1966) reported that the temperature-salinity relationships in the Central Waters were much better described by a curve of constant density ratio (Rρ = αΔT/βΔS) than by a straight line. His res...
The Relationship between Downward Irradiance and Upper Ocean Structure
Downward Irradiance Upper Ocean Structure
2009/2/9
The relationship between downward irradiance and upper ocean structure has been studied using a numerical model. Two general classes of irradiance parameterizations were utilized. The first (case I) e...
The Relationship Between Deep Ocean Currents and Winds East of Barbados
Deep Ocean Currents Winds Barbados
2009/2/7
Observations of currents collected at the POLYMODE array III cluster C (16°N, 54°W) are compared with radiosonde winds measured at Barbados (13°N, 62°W) using a linear response analysis. The winds and...
The Relationship between Vertical, Diapycnal, and Isopycnal Velocity and Mixing in the Ocean General Circulation
Ocean General Circulation vertical velocity diapycnal velocity
2009/1/10
On ocean general circulation scales, vertical velocity w is extremely small, O(10−5) smaller than the horizontal velocity in scale. Nevertheless, it is of great importance to advective–diffusive...
Ocean Radar Backscatter Relationship with Near-Surface Winds：A Case Study during FASINEX
Ocean Radar Backscatter Frontal Air-Sea Interaction Experiment Near-Surface Winds
2008/12/30
A case study of ocean radar backscatter dependence on near-surface wind and wind stress is presented using the data obtained on 18 February 1986 during the Frontal Air-Sea Interaction Experiment. Our ...
On the Relationship between Subduction Rates and Diabatic Forcing of the Mixed Layer
Subduction Rates Diabatic Forcing Mixed Layer
2008/12/24
The transport of mass between a mixed layer, exposed to mechanical and thermodynamic forcing, and an adiabatic thermocline is studied for gyre-scale motions. It is shown that if the mixed layer can be...
The Relationship between Variations in the Gulf of Mexico Loop Current and Straits of Florida Volume Transport
Mexico Loop Current Florida Volume Transport Loop Current
2008/12/18
Twelve years of monthly mean positions of the northern boundary of the Loop Current in the eastern Gulf of Mexico from satellite and in situ data have been compared with coincident 1977–1988 estimates...
The Relationship between Water Mass Formation and the Surface Buoyancy Flux, with Application to Phillips’ Red Sea Model
Water Mass Formation Surface Buoyancy Flux Red Sea Model
2008/12/12
A buoyancy flux across the sea surface between the outcropping of isopycnals must be balanced by a subsurface diapycnal buoyancy flux. If this flux were only advective, its derivative with respect to ...
High-Frequency Internal Waves at 0°, 140°W and Their Possible Relationship to Deep-Cycle Turbulence
surface mixed layer High-Frequency Internal Waves Deep-Cycle Turbulence
2008/12/9
An analysis of a moored time series at 0°, 140°W from November to December 1991 found a nighttime enhancement of isotherm displacement variance and of zonal velocity variance below the surface mixed l...
Exploring the Relationship between Eddy-Induced Transport Velocity, Vertical Momentum Transfer, and the Isopycnal Flux of Potential Vorticity
Eddy-Induced Transport Velocity Vertical Momentum Transfer Isopycnal Flux
2008/10/31
Gent et al. have emphasized the role of the eddy-induced transport (or bolus) velocity as a mechanism for redistributing tracers in the ocean. By writing the momentum equations in terms of the isopycn...
A Relationship between the Bowen Ratio and Sea–Air Temperature Difference under Unstable Conditions at Sea
Bowen Ratio Sea–Air Temperature Unstable Conditions
2008/10/23
At the air–sea interface, estimates of evaporation or latent heat flux and the Monin–Obukhov stability parameter require the measurements of dewpoint (Tdew) or wet-bulb temperature, which are not rout...