Poole 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 1.5m / 5.1ft). 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.

Poole Harbour is one of the largest natural harbours in the world by surface area — roughly 36 square kilometres of sheltered, shallow water occupying a drowned river valley behind a narrow shingle entrance that barely exceeds 100 metres at its narrowest point between the Sandbanks peninsula and the Shell Bay shore on the Studland side. The geography creates a tidal situation that baffles visitors who arrive expecting standard English Channel conditions. Outside the harbour entrance, in the English Channel off Swanage and Studland Bay, the tidal range is a normal 1.5 to 2.0 metres — enough to shift the character of the beach and the approach to the Studland sand dunes across a day, but nothing unusual for the south coast. Step inside the harbour entrance and the story changes completely. The restriction at Sandbanks limits how fast water can flow in or out, and the harbour's large surface area means the volume of water that needs to move to fill or drain it is substantial. The result is that the harbour simply cannot keep pace with the ocean tide outside. The range inside Poole Harbour on a spring tide is approximately 0.5 to 0.6 metres — the tidal signal has been attenuated by more than two-thirds within a few hundred metres of the entrance. Inside the harbour, tide is almost irrelevant for practical purposes. What this means in practice: the extensive shallows of Holes Bay to the north and Lytchett Bay to the northwest dry out at low water but the variation across the tidal cycle is small enough that dinghy sailing and kayaking remain viable across a wide range of states. The 150 or so islands and mudflat islets within the harbour — including Brownsea Island, the largest, with its National Trust woodland and Scouting historical significance — sit in stable, low-energy water. The Sandbanks channel between the entrance and the main harbour, however, is a very different proposition. On spring tides the ebb and flood through this 100-metre gap runs at 3 to 4 knots — currents that are immediately obvious to anyone swimming near the entrance, kayaking across the channel, or watching the Sandbanks chain ferry work against the flow. The Sandbanks chain ferry runs continuously across this gap, connecting the Sandbanks peninsula road to Shell Bay and Studland on the Isle of Purbeck — a five-minute crossing that would be a long drive around without it. The ferry is designed to handle the current. Swimmers and kayakers crossing the channel outside the ferry lanes should be aware that the current is fast and the commercial ferry, along with private motor craft, uses the same narrow water. Poole town itself sits on a peninsula inside the harbour, the old quay lined with restaurants, chandleries, and the Poole Pottery building. The low tidal range means the quayside stays accessible throughout the cycle — there is no stranding at low water in the way that would affect a harbour with a 4-metre range. The water taxis running between Poole Quay, Brownsea Island, and Sandbanks operate on this basis. Studland Bay, just outside the harbour to the east, offers a different experience — the full English Channel range on a sheltered, northwest-facing sand beach with the Old Harry Rocks chalk stacks marking the Handfast Point headland and the beginning of the Jurassic Coast. The Jurassic Coast designation covers 155 kilometres of Dorset and Devon shoreline, all of it accessible by the South West Coast Path. At Studland, the beach at low water gives access to sandbars and shallows that are submerged at high — a particular draw for families and shore anglers targeting bass in the gullies between the sand ridges on the flood tide. Portland Bill, 20 kilometres west along the coast past Weymouth, generates the Portland Race — a zone of tidal overfalls where the stream running around the Bill at up to 7 knots on springs meets itself and creates standing waves. The Race is marked on Admiralty charts and is avoided by all small craft, particularly near springs on a fresh wind-against-tide day when the overfalls can be dangerous. Chesil Beach, the 18-kilometre tombolo connecting Portland to the mainland, is the classic Dorset shore-angling location — steep shingle with deep water immediately off the beach, producing good bass, cod, and dogfish results in autumn and winter. The Fleet lagoon behind Chesil is another enclosed, nearly atidal water body similar in principle to Poole Harbour, though much smaller and without a significant harbour current. Tide predictions for this page come from Open-Meteo Marine, a global gridded model — model-derived, not from a local gauge. Accuracy is typically within plus or minus 45 minutes on timing and 0.2 to 0.3 metres on height. For Poole specifically, the outside-harbour and inside-harbour tide conditions differ significantly; the model prediction represents the broader Poole Bay and harbour area. Authoritative data comes from the UK Hydrographic Office Admiralty Tide Tables and the National Tidal and Sea Level Facility (NTSLF).