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Sneaker Waves Explained: Why the Ocean Can Surprise You at Any Tide

A sneaker wave is an unusually large wave that surges much farther up the beach, or over rocks and jetties, than every wave before it — often with no obvious warning. They're a leading cause of beach fatalities on parts of the Pacific coast.

Why they happen

Ocean waves arrive in groups, or "sets," and the size within a set varies. A sneaker wave usually results from multiple swell trains overlapping and briefly reinforcing each other, sometimes combined with distant storm energy that isn't obvious from the beach on an otherwise calm day. They aren't a tide phenomenon specifically — the risk exists at any tide stage, though a rising tide can leave less dry beach as a margin for error.

Why they're so dangerous

People misjudge how far back is "safe," especially on rocks, jetties, or low bluffs where the wave's reach isn't obvious until it arrives. The backwash from a large sneaker wave is often stronger than people expect and can sweep someone off their feet, off a rock, or into cold water with a swift undertow, all in a few seconds.

Where they're most common

Sneaker waves are most associated with the Oregon, Washington, and Northern California coasts, especially near river mouths, jetties, and rocky headlands, and especially during the fall and winter storm season — but the underlying mechanism can happen anywhere large swell reaches a beach.

How to stay safe

Related: rip current safety, storm surge vs. tide.