The Closure of a Shallow Tidal Inlet Promoted by Infragravity Waves
Tidal inlets connect the ocean to inner water bodies and are present worldwide. Shallow inlets display fast morphological changes, due to complex interactions between tides, waves, and shallow depths. Their closure is commonly observed under storm waves, but the underlying processes remain only part...
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Veröffentlicht in: | Geophysical research letters 2019-06, Vol.46 (12), p.6804-6810 |
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