Northward flowing boundary currents are identified as the major dynamical elements. At the northern boundary, the eastern current follows the geometry, eventually turning back to the south. At approximately 26N and the western wall the two boundary currents collide. At the collision site, the denser eastern current subducts under the western boundary current. The subduction forces the western boundary current eastward into the interior.
Convection communicates the surface fluxes to the downwelled plume and intermediate water forms.
The estimated rate, 0.11 Sv, agrees with previous estimates. The resultant geostrophic eastward cross-channel flow interacts with the boundaries, and creates upwelling and surface topography spatial patterns which drive the coastal jets. Upwelling-induced vortex stretching dominates the vorticity balance, and governs the separation of the western boundary current from the western wall. The process ceases in the summer.