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The influence of wind on the surface waters of Alberni Inlet Farmer, David Malcolm
Abstract
Observations of wind, current and surface layer thickness in Alberni Inlet have helped elucidate some of the ways in which the system responds to a surface stress. The energy of the wind and also the current at 2 meters depth is strongly diurnal. Cross-spectral analysis has shown that the two are closely coupled at this frequency. On the basis of simple time scale considerations I have used phase angles between wind and current to estimate a bulk eddy viscosity for the upper two or three meters of the inlet. This method has yielded values between 1 and 10 cm²/sec. On the other hand most of the energy associated with changes in the surface layer thickness is of significantly lower frequency. Strong up-inlet winds induce a sudden thickening in the surface layer at the inlet head and the disturbance appears to propagate back down the inlet suffering an attenuation as it travels. The return to equilibrium can take several days. A simple two-layer frictional model is able to explain much of what is observed and can be used to predict the surface layer thickness on the basis of measured wind speeds.
Item Metadata
Title |
The influence of wind on the surface waters of Alberni Inlet
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Creator | |
Publisher |
University of British Columbia
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Date Issued |
1972
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Description |
Observations of wind, current and surface layer thickness in Alberni Inlet have helped elucidate some of the ways in which the system responds to a surface stress. The energy of the wind and also the current at 2 meters depth is strongly diurnal. Cross-spectral analysis has shown that the two are closely coupled at this frequency. On the basis of simple time scale considerations I have used phase angles between wind and current to estimate a bulk eddy viscosity for the upper two or three meters of the inlet. This method has yielded values between 1 and 10 cm²/sec.
On the other hand most of the energy associated with changes in the surface layer thickness is of significantly lower frequency. Strong up-inlet winds induce a sudden thickening in the surface layer at the inlet head and the disturbance appears to propagate back down the inlet suffering an attenuation as it travels. The return to equilibrium can take several days.
A simple two-layer frictional model is able to explain much of what is observed and can be used to predict the surface layer thickness on the basis of measured wind speeds.
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Genre | |
Type | |
Language |
eng
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Date Available |
2011-03-17
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Provider |
Vancouver : University of British Columbia Library
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Rights |
For non-commercial purposes only, such as research, private study and education. Additional conditions apply, see Terms of Use https://open.library.ubc.ca/terms_of_use.
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DOI |
10.14288/1.0053230
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URI | |
Degree | |
Program | |
Affiliation | |
Degree Grantor |
University of British Columbia
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Campus | |
Scholarly Level |
Graduate
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Aggregated Source Repository |
DSpace
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Item Media
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Rights
For non-commercial purposes only, such as research, private study and education. Additional conditions apply, see Terms of Use https://open.library.ubc.ca/terms_of_use.