Haida eddies are characterized as transient, mesoscale anticyclonic eddies their formation has been documented to be dependent on baroclinic instabilities from alongshore wind reversals, equatorial Kelvin waves and bottom topography.
Their formation has been documented to be dependent on baroclinic instabilities from alongshore wind reversals, equatorial Kelvin waves and bottom topography. Haida eddies are characterized as transient, mesoscale anticyclonic eddies.
Haida eddies are characterized as transient, mesoscale anticyclonic eddies. Their formation has been documented to be dependent on baroclinic instabilities from alongshore wind reversals, equatorial Kelvin waves and bottom topography.
Haida eddies are characterized as transient, mesoscale anticyclonic eddies. Their formation has been documented to be dependent on baroclinic instabilities from alongshore wind reversals, equatorial Kelvin waves and bottom topography.