Slope Water Interaction Workshop

23-24 August, 2000

Clark Laboratory, Woods Hole Oceanographic Institution

 


Abstract

Overviews

Observations and Models

 

Fig. 4: Remotely sensed sea surface temperature near the end of the cruise. The black lines mark the last repeat of the intensive survey. The instability seen in Fig. 3 has now grown into a warm tendril that extends well onto the Bank.