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diameters of the eddies.

 

These results suggest that further observations are necessary to resolve possible eddy structures over the Arctic selves, and also to determine both their vertical structure and their evolution as they pass offshore to the shelfbreak.

 

REFERENCES

 

Aagaard, K., L.K. Coachman, and E. Carmack, 1981: On the halocline of the Arctic Ocean. Deep-Sea Res., 28A, 529-545.

 

Chapman, D. C,, and G. Gawarkiewicz, 1997: Shallow convenction and buoyancy equilibration in an idealized coastal polynya. J. Phys. Oceanogr., 27, 555-566.

 

Gawarkiewicz, G., and D. C. Chapman, 1995: A numerical study of dense water formation and transport on a shallow, sloping continental shelf. J. Geoghys. Res.-Oceans, 100, 4489-4507.

 

McDonald, N. R., 1993: Topographic dispersal of bottom water. J. Phys. Oceanogr., 23,954-969.

 

Meilling, H., and R. M. Moore, 1995: Modification of halocline source waters during freezing on the Beaufort Sea shelf: evidence from oxygen isotopes and dissolved nutrients. Cont. Shelf Res., 15, 89-113.

 

 

 

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