A study of the oceanographic structure in British Columbia inlets and some of the determining factors
Fresh water entering the inlets moves seaward, mixing with and entraining salt water from below. On the assumption that horizontal advection of salt is balanced by vertical diffusion, the magnitude and variation in time and space of the diffusion coefficient are determined by numerical evaluation of...
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| Language: | English |
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University of British Columbia
2012
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| Online Access: | http://hdl.handle.net/2429/40675 |