Tides are the rise and fall of sea level caused by the gravitational pull of the Moon and the Sun, combined with Earth’s rotation. But they don’t simply slosh back and forth — they travel as waves across ocean basins, shaped by local water depths, coastlines, and seabed features. This is called dynamic tidal theory.
Instead of two static bulges, tides move like rotating waves. Ocean basins act like resonant bowls, bending and steering these waves. Earth’s rotation (Coriolis force) adds a twist, producing rotating systems centered on amphidromic points..
Unlike wind or solar, tides are perfectly predictable years ahead. That makes them a powerful renewable resource.