You see them a lot here on Kiel fjord when it’s windy, and this is what they looked like last Saturday: Foam stripes than run parallel to the coast for as long as the coast is a sea wall (or at least something fairly straight). What’s going on there?
I have seen them over and over again, and the most common explanation that people have is Langmuir circulation, which i don’t actually think it is (and I show you some evidence for why I don’t think they are Langmuir circulation in this blog post). The stripes we see here are nowhere near parallel to the wind direction. Last Saturday, they were pretty much perpendicular.
So I think there is just a surface convergence there, parallel to the coast, probably related to the typical wavelength. So the question should probably be: Why is there a convergence parallel to the coast independent of the wind direction? What do you think?