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Coastal Countercurrent and Mesoscale Eddy Formation by Tidal Rectification near an Oceanic Cape
Coastal Countercurrent Mesoscale Eddy Formation Tidal Rectification Oceanic Cape
2009/1/9
Cape St. James is an extensive triangular-shaped promontory located in a tidally energetic region at the southern tip of the Queen Charlotte Islands approximately 150 km off the mainland coast or Brit...
Numerical Simulations of a Buoyancy-Driven Coastal Countercurrent off Vancouver Island
Numerical Simulations Buoyancy-Driven Coastal Vancouver Island
2008/7/8
A three-dimensional prognostic numerical model has been developed to study the ocean circulation around Vancouver Island, British Columbia. In a series of simulations, the model is applied to examine ...