Poincare Waves and Kelvin Waves in a Circular Lake
When wind blows over a stratified lake an interface tilt is often generated, and internal waves usually appear after the wind stops. Internal waves in lakes are studied in many literatures, but most assume a hydrostatic pressure balance. In this thesis we discuss the internal Poincare waves and Kelv...
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| Language: | en |
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2009
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| Online Access: | http://hdl.handle.net/10012/4265 |