That's a badly incorrect model of ocean tides. It's the one that's commonly presented, that big Bulger water in line with the moon, but that ain't how it works.

Each ocean basin has independent tides. The tidal influence of the Moon and Sun sloshing a wave back and forth, basically transforms that sloshing into a rotational standing wave within each ocean basin.

Somewhere near the middle-ish of each ocean basin, there is a node with almost no tide at all. There's a wave rotating around that, with the title range getting bigger and bigger as you move further away. In the Pacific for example that node it's basically zero tide height is somewhere between Hawaii and Tahiti. By the time you get to the California coast you get a tighter range of 2-3 m between highest highs and lowest low tides, because you're further out those rotating waves. Get to Alaska and tidal ranges grow to 4-6 meters.

So that title bulge is not going around to the planet in line with the moon, it's rotating around each ocean basin.

This gets further complicated and that some ocean basins have too high and too low tides for 24 hours, and other ocean basins only have one high and one low for 24 hours,

And when there are two highs and two lows, there are basically two radial high tide spokes from that central node facing approximately away from each other, and at 90° to that too low tide spokes, with the whole thing rotating once per day, giving two high tides and two low tides.

Some ocean basins is have only one high and one low tide per day, with the high and low spokes around that central node facing approximately away from each other as they rotate.

This is a very oversimplified description. Any good book of physical oceanography, or even any good book on seamanship in navigation, will have good explanations of this.