Journal of Fluid Mechanics

The generation of continental shelf waves

J. K.  Adams a1 and V. T.  Buchwald a1
a1 School of Mathematics, The University of New South Wales, Kensington, N.S.W. 2033

Article author query
adams jk   [Google Scholar] 
buchwald vt   [Google Scholar] 


Assuming zero divergence, the equations of forced long waves in a uniformly rotating, homogeneous ocean are reduced to a single partial differential equation for the stream function. A shelf of exponential slope between a rigid continent and a sea of uniform depth is taken as a model, and certain other assumptions are made which appear physically reasonable. Calculations made on the basis of this simplified theory are in good qualitative agreement with observations of shelf waves, indicating that these waves are generated by the stress of the longshore component of the geostrophic wind.

(Published Online March 28 2006)
(Received June 18 1968)