Abstract:
A laboratory model of wintertme cooling over a continental shelf has a water surface cooled by air in an annular rotating tank. A flat
shallow outer "continental shelf" region is next to a conical "contiental slope" bottom and a flat "deep ocean" center. The shelf flow
consists of cellular convection cells descending into a region with very complicated baroclinic eddies. Extremely pronounced fronts
are found at the shelf break and over the slope. Associated with these are sizable geostrophic currents along the shelf and over shelf
break contour. Eddies are particularly energetic there. Cooling rate is compared with temperature difference between "continental
shelf" and "deep ocean". Scaling considerations produce an empirical best fit formula for temperature difference as a function of
cooling rate. This produces a relatively straight regression line over a wide range of rotation rates, shelf depths and cooling rates. If
this formula is valid for the ocean, water over continental shelves will be much colder due to constraints imposed by rotation of the
earth than if the fluid were not rotating.
