Tidal resonance

In oceanography, the phenomenon of Tideresonanz is best documented by the Tidebewegung in the Bay of Fundy.

A (high ) running into the bay tidal wave is reflected at the end of the bay. It 's true, the runtime required by the tidal wave to travel from the mouth into the bay and back again, with the time interval between two successive high water levels match. This temporal coincidence with the result that the water surface elevations in the bay are amplified in the rhythm of the tide. In the Bay of Fundy are measured with up to 21 m height difference between high tide and low tide the world's largest Tidenhübe.