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Isle of Wight

The Isle of Wight sits at the centre of the Solent system, and its tidal regime is one of the most complex in northern Europe. On the island's north and east coasts — Cowes, Ryde, and the eastern Solent — the tidal wave that enters the English Channel diffracts around both ends of the island and arrives from opposite directions at slightly different times. The result is the famous double high water: a main high tide, a partial ebb, a second stand, and then the full ebb. At Ryde the HW period can last 2–3 hours, making harbour operations and beach planning fundamentally different from anywhere with a clean single peak. On the island's south coast — Ventnor and the English Channel shore — the double-HW effect disappears and the regime simplifies to a single high water with a spring range of only 2.8 m, roughly half the Solent's 4.5 m. The contrast between north and south coasts, separated by just 10 km of island, is unusual globally. Cowes, on the west Medina entrance, has been the world centre of yacht racing since the Royal Yacht Squadron was founded in 1815; Cowes Week in August is the largest sailing regatta in the world by entry. The island's tidal complexity, its Solent setting, and its varied coastline make it a place where understanding the tide table produces real, practical reward.

Isle of Wight tide stations

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Tide times are guidance for planning, not navigation. See the methodology page for how the data is built.