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Water motion in the barotropic mode, directly forced by suddenly imposed wind stress, is investigated in basins with arbitrary topography, but paying special attention to long basins, in which the dep...
An Ekman Model of Coastal Currents in a Lake or Shallow Sea
Ekman Model Coastal Currents Shallow Sea
2009/4/2
Coastal currents are investigated by use of asymptotic solutions in a steady-state barotropic lake or shallow sea of variable depth, with only vertical eddy viscosity and zero Rossby number. Earlier w...
Transient Long-Wave Response for a Multiple-Island System
Transient Long-Wave Response Multiple-Island System
2009/4/2
An interpretation of the tsunami response at the Hawaiian island of Kauai has been carried out utilizing simple geometric representations which include the three-island system of Kauai, Niihau and Oah...
Circulation Patterns Near the Tail of the Grand Banks
Circulation Patterns Tail of the Grand Banks
2009/4/2
Dynamic topographies for the region surrounding the tail of the Grand Banks have been examined for the years 1922–65, in an attempt to define the characteristics of the eddies and meanders typical of ...
A Numerical Investigation of Arctic Ocean Dynamics
Numerical Investigation Arctic Ocean Dynamics
2009/4/2
A barotropic numerical model of the Arctic Ocean is formulated to include irregular basin shape, variable bathymetry, lateral friction, bottom drag, and nonlinear advection terms. Source-sink distribu...
Thermal Communication Between the Sea Surface and the Lower Troposphere
Thermal Communication Lower Troposphere Sea Surface
2009/4/2
Seasonal mean sea surface temperatures and 1000–700 mb thicknesses are correlated by pattern and also for 5° squares over the eastern North Pacific in order to find out more about bulk heat exchange b...
Monte Carlo Calculations of the Polarization of Radiation in the Earth's Atmosphere-Ocean System
Monte Carlo Calculations Polarization of Radiation Earth's Atmosphere-Ocean System
2009/4/2
The degree and direction of polarization, the ellipticity, and the radiance of the radiation at various levels in the atmosphere and ocean are calculated by a Monte Carlo method which includes all ord...
Experiments with Monomolecular Films on the Surface of the Open Sea
Monomolecular Films Experiments the Open Sea
2009/4/2
Experiments with monomolecular films were conducted in the axis of the Gulf Stream, east of Miami, in June 1972, to examine the feasibility of spreading and maintaining a continuous partially-polymeri...
Some Problems Associated with Wind Drag and Infrared Images of the Sea Surface
Wind Drag Sea Surface Infrared Images
2009/4/2
It is argued that there should be a close connection between fluctuations in infrared images of the sea and fluctuations in wind drag on the sea. The critical regions of wind speed, temperature, and s...
Bispectra and Cross-Bispectra of Temperature, Salinity, Sound Velocity and Density Fluctuations with Depth off Northeastern Japan
Temperature Salinity Sound Velocity Density Fluctuations
2009/4/2
Off northeastern Japan, depth profiles of temperature, salinity, sound velocity and density show considerable structure between 30 and 240 m. The structure is asymmetric with respect to the mean and t...
Measurements of the vertical component of the temperature gradient in Powell Lake show phenomena similar to those observed in the ocean. The gradient is an irregular function of depth, with temperatur...
Gulf Stream Eddies：Recent Observations in the Western Sargasso Sea
Gulf Stream Eddies Western Sargasso Sea
2009/4/2
A cyclonic Gulf Stream eddy was observed in the western Sargasso Sea by satellite infrared measurements and later confirmed by ship measurements. Fourteen months of observations indicate that the eddy...
Vertical mixing in the ocean affects the formation of water masses as well as the vertical distribution of nutrients and dissolved substances. This study is an investigation of the vertical mixing in ...
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...
Wind–Induced Baroclinic Motions at the Edge of the Continental Shelf
Wind–Induced Baroclinic Motions Continental Shelf
2009/4/2
In a two-layer model of stratified fluid flow, motions in the internal mode are governed by the distribution of an equivalent depth he. For a typical continental shelf, the distribution of he with dis...