A one-dimensional mixed-layer model is used to simulate observations made by a NOAA buoy in the Gulf of Mexico during Hurricane Eloise. The model-predicted SST, mixed-layer depth, and inertial current agree favorably with the observations. In addition, model experiments demonstrate the importance of the veering of the wind vector during the passage of the eye to the amplitude of the inertial current generated by the wind and the extent of vertical mixing. |