Year

1978

Degree Name

Master of Science

Department

Department of Mathematics

Abstract

A theoretical model for the upwelling of homogeneous water over -a bottom profile is considered. The model consists of a north-south coastline in the southern hemisphere with a continental shelf and slope to the east. A wind stress is assumed to have acted on the surface for a sufficient length of time to produce steady-state motion.

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Unless otherwise indicated, the views expressed in this thesis are those of the author and do not necessarily represent the views of the University of Wollongong.