6 min read
Waves break over sand bars, ridges of sand a bit off the shore. Where a bar is shallow, the wave breaks and forms a peak. Deeper gaps between bars are channels, where the water drains back out. Because sand moves, the best banks change with every big swell and every season: a corner that was perfect in March can be flat water by June.
The bottom is rock or coral, so it never moves. The wave breaks in the same place every time, which makes reefs more predictable and often hollower. They also make mistakes cost more: shallow, sharp, sometimes with sea urchins. Tide matters a lot. A reef that is a metre under water at high tide can be nearly dry at low.
A headland sticks out into the swell. The swell bends round it (refraction) and peels along the point, often for a long distance in one direction. Rides of 200 m and more are normal at the best ones.
Drawing: Swell lines bend around a headland to line up with the shallow bottom, and the wave peels along it.
In the app: The spot guide on every page shows the swell window and the best wind and tide. "Now" under the dials shows how today's conditions compare.