Tidally induced internal motion in an Arctic fjord
The internal response in a stratified, partially enclosed basin subject to semi-diurnal tidal forcing through a narrow entrance is investigated. The site is located above the critical latitude where linear internal waves of lunar semi-diurnal frequency are not permitted to propagate freely. Generati...
| Päätekijät: | , |
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| Aineistotyyppi: | Artikkeli |
| Kieli: | English |
| Julkaistu: |
Copernicus Publications
2014-01-01
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| Sarja: | Nonlinear Processes in Geophysics |
| Linkit: | http://www.nonlin-processes-geophys.net/21/87/2014/npg-21-87-2014.pdf |