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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...
Probability Distribution of Concentrations Measured in the Wake of a Continuous Point Source in Coastal Currents
Continuous Point Source Coastal Currents
2009/3/7
A generalized statistical model is proposed to determine the probability density function of the concentration history measured at a fixed point in the wake of a continuous point source in coastal cur...
Baroclinic and Barotropic Instabilities of Coastal Currents
Baroclinic Coastal Currents Barotropic Instabilities
2009/2/9
The two-layer baroclinic instability model of the California Undercurrent from Mysak (1977) is modified to investigate the effects of the lateral boundary conditions on the stability properties of the...
Summertime Coastal Currents in the Northeastern Gulf of Mexico
Summertime Coastal Currents Northeastern Gulf Mexico
2009/1/21
Observations of currents and temperature at a mooring on the 18 m isobath, 30 km south of the Florida shoreline, are discussed for the 31-day period 15 August–15 September 1978. Tidal currents, having...
Amplitude–Wavelength Relations of Nonlinear Frontal Waves on Coastal Currents
Amplitude–Wavelength Coastal Currents Nonlinear Frontal Waves
2009/1/5
Nonlinear, dispersive perturbations are applied to a single layer, geostrophic, density current of zero potential vorticity, which flows along a vertical wall (coast) and is bounded by a free streamli...
Finite-Amplitude Long Waves on Coastal Currents
Finite-Amplitude Long Waves Coastal Currents
2008/12/27
Two models of coastal currents are described that allow fully nonlinear wavelike solutions for the limit of long waves. The first model is an adaptation of a model used by Yi and Warn for finite-ampli...
Boundary Layer Control of Buoyant Coastal Currents and the Establishment of a Shelfbreak Front
Boundary Layer Control of Buoyant Coastal Currents and the Establishment of a Shelfbreak Front
2008/7/4
The bottom boundary layer exerts a powerful control over buoyant coastal currents that contact the bottom, providing a mechanism for trapping density fronts along isobaths. Recent observations suggest...