A lot of rip currents happen when the shore forms a U or V shape. Even a small variation can make a difference. When the wave comes in it comes at a straight line. Now, as the line – hits the curved parts of the U the water continues going forward and a little bit in, the water is deflected in a little then continues forward. Once the water hits the furthest inland portion, it has accumulated a lot more water in that area and all has to go back out. Since there isn’t anything blocking the way, a large current of water flows back out straight from this point (the bottom of the U in my example).
To be clear, it doesn’t have to be a U shape, just a section where the shore is curved and will redirect the flow to the center of the curve.
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