Cardiff 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.

Conditions as of 05:00 local time. Refreshes daily.

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.

Last spring tide on Sat 02 May (range 10.1m / 33.1ft). Next neap on Fri 08 May.

Spring tides cluster around new and full moons (biggest swings). Neap tides land on quarter moons (smallest swings). See the spring tide and neap tide glossary entries for the why.

Cardiff sits on the northern shore of the Bristol Channel, at the point where the Severn Estuary narrows toward the Severn bridges, and the tidal range here is one of the largest in the world. Spring tides at Cardiff regularly reach 12 to 14 metres between low and high water. To put that in context: at low water springs, the foreshore east and west of Cardiff Bay exposes broad mudflats stretching hundreds of metres from the sea wall; six hours later, the same ground is under several metres of water. There is no other capital city in Europe where the tidal range is this large, and it shapes everything about how Cardiff's waterfront works. Cardiff Bay itself is now an impounded freshwater lake — the Cardiff Bay Barrage was completed in 1999, sealing the mouths of the Rivers Taff and Ely to create a permanent water level and eliminate the vast mudflat that previously dominated the bay at low tide. The barrage has a fish pass, a lock for vessels wanting to transit between the bay and the open Severn, and sluice gates that discharge freshwater into the estuary. Outside the barrage, the tidal Severn continues on its natural 12 to 14 metre cycle. The barrage decision was controversial for exactly that reason: the Severn Estuary SSSI, which includes the intertidal mudflats, is one of the most important bird habitats in the UK — tens of thousands of dunlin, knot, redshank, and curlew depend on the mudflats for feeding during winter. The sealed bay removed a significant stretch of that habitat. What was gained is a stable waterfront suitable for the Senedd (Welsh Parliament), the Wales Millennium Centre, and the marina developments that transformed Cardiff's docklands economy in the 2000s. West of Cardiff, the coast at Barry and Penarth remains openly tidal — the mudflats exposed at low water there give an idea of what the bay's foreshore looked like before the barrage. The spring tide low at Barry or Penarth is a dramatic low, with the foreshore extending far and the channel shipping fairway marked by buoys standing in shallow water between the exposures. For kayakers and paddleboarders, the tidal currents in the outer Severn are a serious planning consideration. The estuary is not just large — it moves fast. The flood tide coming up the channel from the Bristol Channel carries significant current, and the narrowing funnel geometry accelerates it further. Experienced sea kayakers paddle the Severn at specific tidal windows, working the eddies and counter-currents behind headlands rather than fighting the main flow. Beginners should stay in the bay on impounded water or paddle close inshore on the ebb with an easy escape route. Anglers fishing the Severn foreshore — from the rocks at Penarth, the shingle at Barry, or the sea walls around Newport further east — time sessions around the flood, when bass, mullet, and flatfish push up over the exposed ground on the rising water. The massive tidal range means that fishing two hours either side of high water from a fixed mark delivers the most productive intertidal zone access. The low-water rocks also produce good wrasse fishing from accessible rocky ground that would be too deep to fish effectively at high tide. The tidal range affects water temperature too: the exposed mudflats heat rapidly on summer low tides, and the water warming over the flats produces thermal stratification on the flood that can trigger bass feeding activity. Photographers working the Bristol Channel foreshore learn the tide table as the primary planning tool — the difference between a shot of a vast mudflat under a winter dawn sky and a shot of flat grey water is the six hours between low and high. The wading birds that feed the mudflats at low tide depart before the flood reaches them, and tracking that movement requires knowing exactly where the tide is in its cycle. Predictions on this page are from Open-Meteo Marine, a global gridded model, typically accurate within plus or minus 45 minutes on timing and 0.2 to 0.3 metres on height. On a 12 to 14 metre range, 0.3 metres of model error is proportionally small — tide height prediction here is relatively reliable in percentage terms even if the absolute uncertainty looks large compared to a microtidal coast. Authoritative data for Cardiff is published by the National Tidal and Sea Level Facility (NTSLF) operating the Cardiff gauge, and in Admiralty Tide Tables volume 1, published by the UK Hydrographic Office.