The height of the tides and the amphidromic point are related, in that the tidal altitude increases as the wave goes away from the amphidromic point.
Tides are very lengthy waves that flow across the water in response to the moon's and sun's powers. Tides start in the ocean and travel to the coasts, where they manifest as the continuous rise and decline of the sea surface.
The amphidromic point and the height of the tides are connected in that the tidal elevation increases as the wave moves away from the amphidromic point.
Therefore, it can be concluded that Heights increase with distance from the amphidromic point.
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