That's a good find. Mostly he talks about ripples with a wavelength of a couple of cm. The formations we've got here are 10 metres or more. In a few places the ~cm ripples were superimposed on the surface of the soft sand accumulations. But maybe our much larger ripples do get a mention in that article right at the end.
"With dry sand, a strong wind begins to wipe out ripples and make larger and regular berms, spaced fairly evenly perpendicular to the wind. These are in reality large ripples. Continued, strong winds can change these rises into undulating dunes that often go far inland."
Another interesting statement from that article, which helps explain why he glossed over our case in that last paragraph.
"There are several possible mechanisms leading to the particular bedforms, and this is an area of
legitimate scientific controversy. The most accepted explanation is that the flow of the overlying fluid (water or air) interacts with the moving sediment grains in a manner that results in a stable shape, or bedform."
I've read the early work by Bagnold that always gets quoted. His interesting observations are.
* When sand grains get picked up by the wind the momentum exchange slows down the boundary layer until it doesn't pick up any more. (Well what gets picked up is equalled by what gets stuck on landing)
* It takes several metres for wind suddenly striking loose sand for it to become saturated. i.e. There's no more wind blown sand moving off a 100 metre wide beach than off a 5 metre wide beach.
* Airborn sand will move quicker if it moves onto a harder surface, the particles bounce better.
So putting that all together to try and sort out why's happening in the photo....
The thickness of the sand accumulations is only a couple of cm. I don't think that's going to affect wind strength when spaced by 10 metres.
but it might be something to do with the boundary layer accelerating and decelerating due to the changing looseness of the sand?
Or maybe it's just something like traffic theory, the sand moves quickly in the gaps until it hits another clump?
I think it's still an area of "legitimate scientific controversy"