This ocean basin model is based on a model of Henry Stommel in The Westward Intensification of
Wind-Driven Ocean Currents
from Transactions of the American Geophysical Union, Vol. 29, No. 2, 1948, pp 202-206.
This model assumes a rectangular ocean basin:
This computer model allows you to experiment with the wind-driven circulation in a homogeneous, rectangular
ocean basin under the influence of surface wind stress, bottom friction, horizontal
pressure gradients and the Coriolis force.