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The influence of bathymetry on coastal upwelling

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posted on 2024-11-11, 11:57 authored by Colin Lill
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.

History

Year

1978

Thesis type

  • Masters thesis

Faculty/School

Department of Mathematics

Language

English

Disclaimer

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.

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