Tamara Barriquand

Continuity Example: Coastal Upwelling/Downwelling

Continuity Example: Coastal Upwelling/Downwelling
Barotropic v. Baroclinic Conditions

Barotropic v. Baroclinic Conditions
Westward Intensification part 1: Sverdrup's Model

Westward Intensification part 1: Sverdrup's Model
The Equations of Motion: The Rossby Number

The Equations of Motion: The Rossby Number
The Equations of Motion: Acceleration Example

The Equations of Motion: Acceleration Example
The Equations of Motion part 2: Forces

The Equations of Motion part 2: Forces
The Equations of Motion part 1: Acceleration

The Equations of Motion part 1: Acceleration
Westward Intensification part 2: Stommel's model

Westward Intensification part 2: Stommel's model
Taking the curl of the velocity to get the Relative Vorticity

Taking the curl of the velocity to get the Relative Vorticity
Vorticity part 3: Potential Vorticity

Vorticity part 3: Potential Vorticity
Vorticity part 2: Planetary Vorticity

Vorticity part 2: Planetary Vorticity
Vorticity part 1: Relative Vorticity

Vorticity part 1: Relative Vorticity
The Equations of Motion: Coriolis Example

The Equations of Motion: Coriolis Example
Subtropical Gyres: Western and Eastern Boundary Currents

Subtropical Gyres: Western and Eastern Boundary Currents
Continuity: The North Atlantic Gyre Example

Continuity: The North Atlantic Gyre Example
The Continuity Equation

The Continuity Equation
The North Atlantic Gyre: Historical Exploration of the Gulf Stream

The North Atlantic Gyre: Historical Exploration of the Gulf Stream