In deep water, water particles orbit—they don’t translate horizontally. A floating boat bobs in place (orbital motion) unless net forces act on it. As waves shoal near shore, orbits flatten and mass transport begins, but several factors keep vessels offshore.
Open-ocean waves (even 3–5 m) exert insufficient force to overcome a vessel’s inertia (mass × acceleration). A 10-tonne boat requires sustained net force to accelerate meaningfully—wind and current dominate.
Wave power ∝ H²T (height² × period). Deep-water swells have long periods but limited height. Breaking waves near shore have high energy but act in the surf zone—where boats avoid being.
Displacement hulls cut through orbits; planing hulls ride atop. Keels, bilge keels, and damping reduce drift. A boat’s waterplane area and damping coefficient resist wave-induced motion.
Anchors embed in seabed; scope (rode length:depth ≥ 5:1) ensures horizontal pull. A properly set anchor holds against combined wave/wind/current forces. Drogues/sea anchors add drag to keep bow into waves.
Skippers avoid lee shores in heavy weather, deploy sea anchors to maintain heading, and choose anchorages with good holding, swing room, and fetch protection. The boat stays; the wave passes.