Southampton tide times

Predictions: Open-Meteo Marine (MeteoFrance SMOC, 0.08° grid) — heights relative to MSL (not chart datum / LAT). Model-derived.

Model-derived from a global ocean grid. Useful indication; expect about ±45 minutes on average vs. a local harmonic gauge, individual stations vary widely. See /methodology for per-region detail. Not for navigation.

Marine-conditions data not available for this station. Wind, swell and water temperature ride along with Open-Meteo Marine; gauge-only stations (e.g. UK EA Flood) publish water level only.

Predictions: Open-Meteo Marine (MeteoFrance SMOC, 0.08° grid) — heights relative to MSL (not chart datum / LAT). Model-derived. · Not for navigation.

The angler tradition for major/minor fishing windows: major ≈3-hour windows around moon transit and opposition; minor ≈2-hour windows around moonrise and moonset. Times are Europe/London local. Folk tradition, not a scientific forecast.

Southampton Water sits at the confluence of two Hampshire rivers — the Test coming down from the north and the Itchen joining from the northeast — in one of the most hydraulically peculiar estuaries on the English coast. The tide here does not behave the way a standard semidiurnal system would lead you to expect. Most British coasts see high water for a relatively brief period before the ebb pulls water away cleanly. At Southampton, high water arrives and then lingers. The water level rises to near the top, retreats slightly, and then rises again — a secondary hump that can hold the water near its peak for three to four hours before the main ebb finally takes over. This double high water, caused by the interaction of two tidal wave paths arriving at the Solent from opposite ends of the English Channel at slightly different times, is the defining hydrographic characteristic of the port. The eastern arm of the tidal wave curves around the Isle of Wight and arrives out of phase with the main flood from the west, and the superposition of those two signals produces the extended high-water plateau. Mean spring range at Southampton is approximately 4.2 metres — genuinely macrotidal, with the gap between the top of the tide and the exposed mud and gravel of the lower estuary wide enough to create a meaningful working window for any activity that depends on water depth. But the double-high pattern means the usable period near the top of the range is substantially longer than the range figure alone suggests. For the liner companies of the early twentieth century, this was the decisive advantage: White Star, Cunard, and Union-Castle could load passengers and provision ships against a prolonged high-water window that would have been a much tighter operation in Bristol or Cardiff. The Titanic sailed from Southampton's Ocean Dock on 10 April 1912 on a combination of a spring tide window and the double-high pattern that gave the departure adequate draught through the relatively shallow water at the dock mouth. Southampton is still the UK's largest and busiest cruise port. The Western Docks handle the major cruise berths; the Eastern Docks contain the ABP container terminal and the vehicle import facility — one of the UK's main car import operations, processing large volumes from European and Asian manufacturers. The view across Southampton Water from the Town Quay or from Hythe on the western shore is almost entirely defined by shipping: car carriers, container ships, cruise liners, and the regular Red Funnel ferries to East Cowes on the Isle of Wight cutting across the working water. For small-boat users, Southampton Water has designated fairways and considerable commercial traffic — the VHF port radio traffic on Channel 12 (Southampton VTS) is a good indication of what is moving and when. The tidal stream runs between 1.5 and 2.5 knots on springs through the main channel, and the double-high pattern means slack water periods are brief and can be harder to judge than in a standard sinusoidal system. Kayakers and paddleboarders use the Itchen and upper Test above the main port area, where commercial traffic thins out, and the tidal range still applies through the river channels. The foreshore at Hamble, on the eastern shore of Southampton Water, is one of the most concentrated sailing and yacht berthing areas in Britain — marinas, boatyards, and the Royal Air Force Yacht Club compressed into a small river mouth with tidal access governed by the same double-high pattern. Anglers fish the groynes and hard standings along the western shore from Marchwood south to Hythe for mullet, bass, flounder, and occasional smoothhound on the flood tide. The mud exposed at low water on the Test shore holds invertebrate food chains that attract significant wader and wildfowl populations — dunlin, redshank, black-tailed godwit, and avocet on the RSPB Eling reserve at the head of the estuary near Totton. The tide predictions on this page come from Open-Meteo Marine, a global gridded ocean model — accuracy is typically within plus or minus 45 minutes on timing and 0.2 to 0.3 metres on height, model-derived not from a local gauge. For Southampton specifically, the double-high-water profile adds complexity: the secondary peak timing varies and the model may not resolve the full shape of the curve with precision. For navigation, harbour operations, or any time-critical use, the UK Hydrographic Office Admiralty Tide Tables for Southampton are the authoritative reference. The National Tidal and Sea Level Facility (NTSLF) operates gauges in the Solent and makes real-time data available online.