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This question is a continuation of my previous question: Questions about the validity of a certain model for tidal resonance at the Bay of Fundy. I need to answer this question in order to return to my previously posted question and test the validity of the model described there.

As far as i understand, the northeastern part of the Gulf of Maine, also called the Bay of Fundy, is the only resonant part of the whole body of water in the Gulf of Maine (which means its natural period is very close to that of the M2 tide component). Therefore, it's logical to assume that the water level at its entrance is fixed to the Atlantic ocean water level, while the tidal range rises higher and higher as we go more and more into the bay; the water level inside the bay is a standing wave with a fixed end at its entrance and a free end at the coasts of its narrow part (this model is called "open harbour"). This description of the situation seems to fit all discussions of tidal resonance phenomenas that i found up to now.

According to this rational, the tidal range at the bay entrance should be similar to that of other coasts near the Atlantic, which is $1-2$$\text{m}$. However, loooking into maps of the tidal range at the bay of fundy, like this one,

enter image description here

reveals that already at the entrance to the bay, the tidal range is about $5-6\text{m}$.

Therefore, my questions are:

  • If the water level at the entrance to the bay of fundy is fixed to the Atlantic ocean water level, why is the tidal range there so large?
  • What are, and this is a general question, the physical effects that govern the enhancement of tidal waves? and i mean other effects than tidal resonance. Is Green's law (which is often used to explain the wave shoaling of tsunamies and other shallow water waves), which might be applied to tidal waves (as they are shallow water waves), relevant here? and if the answer is yes, than why is it relevant only to the Gulf of Maine and not to other US/Canadian coasts?
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    $\begingroup$ The tide at the entrance to the Bay is not the tide of the North Atlantic. The entire Gulf of Maine is part of the resonance $\endgroup$ – arkaia Jun 6 at 15:15
  • $\begingroup$ @arkaia - thanks for the comment! If the entire Gulf of Maine is part of the resonance, can you recommend a website which gives reliable data on its period of resonance? And can you answer my second on Green's law? Because in wikipedia article on tidal resonance Green's law is mentioned... $\endgroup$ – user2554 Jun 7 at 12:24
  • $\begingroup$ I doubt is the main factor. Here are some notes from Garrett: gfd.whoi.edu/wp-content/uploads/sites/18/2018/03/… $\endgroup$ – arkaia Jun 7 at 13:05
  • $\begingroup$ From David Brooks (Texas A&M): "When the tidal wave inside the Gulf ebbs and flows back to the Atlantic to begin another cycle, it arrives at the Northeast Channel and the offing of the banks almost exactly in step with the next Atlantic tidal impulse, which sweeps past the channel entrance at the propitious moment when the waters inside can most easily accept the next inrush. " $\endgroup$ – arkaia Jun 7 at 13:12
  • $\begingroup$ The Northeast Channel is likely the main constraint. en.wikipedia.org/wiki/Gulf_of_Maine#/media/… $\endgroup$ – arkaia Jun 7 at 13:15
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The Bay of Fundy is shaped like a funnel, which amplifies the tidal magnitude, as the water is "squashed" into the bay. There are several other funnel-shaped bays with a large tidal amplitude around the world, e.g. Bristol Channel in Wales, UK.

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    $\begingroup$ your answer partially explains why the tides are amplified inside the bay, but doesn't explain why the tidal range is large at the entrance to the bay, so it doesn't address my question. $\endgroup$ – user2554 Jun 7 at 12:28

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