Final answer:
Resonance tides in ocean basins have larger ranges than in lakes due to factors like the local shoreline's topography and the bathymetry of the ocean floor, as well as basin resonance with tidal forces, exemplified by the Bay of Fundy's dramatic tidal range.
Step-by-step explanation:
The resonance tides produced in basins open to the ocean, such as the Bay of Fundy, usually have larger ranges than those for lakes due to the interaction of gravitational tidal forces, earth's rotation, and local geographic features. The topography of the local shoreline and the bathymetry of the ocean floor deeply influence the range of tides. In the case of the Bay of Fundy, the peculiar shape and depth of the basin amplify the natural tidal bulges caused by the moon's gravitational pull, leading to extreme high and low tides—up to 16.3 meters. Lakes, on the other hand, are generally smaller and more contained, limiting the extent of the tidal forces' effect.
In addition, the presence of land masses, oceanic friction, and the variable depth of ocean basins contribute to the complexity of the tidal patterns observed. These factors are less significant in confined bodies of water like lakes, which is why their tidal range is less dramatic. The Bay of Fundy's extreme tidal range is also a result of its resonance with the natural frequency of the tidal forces, effectively enhancing the tide's range.