Whitstable 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 00:00 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 Mon 04 May (range 3.9m / 12.8ft). Next neap on Sun 10 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.

Whitstable is on the Thames Estuary, about 80 kilometres east of London on the north Kent coast, and it has become the default London weekend escape for people who want a functional seaside rather than a theme-park one. The tidal range is macrotidal: mean spring range around 4.8 metres, neaps dropping to 3.2 m. Low water retreats far enough that the foreshore sometimes seems to disappear entirely — the seabed exposed is stony and muddy in parts, sandy in others, and this is where the oysters grow. Whitstable is synonymous with native oysters (Ostrea edulis), cultivated here since Roman times. The oyster beds are tended by local fishermen; the town holds its oyster festival each July. The catch cycle is partly tidal — oysters are harvested on low water, when the beds are accessible by flat-bottomed punt. Visitors can buy oysters at the harbour stalls from early morning; the freshest are eaten immediately at the beach wall with lemon and Tabasco. The beach is predominantly shingle, with some sand revealed at low water on the western stretches. Swimmers favour the incoming tide from mid-ebb onwards — the receding water leaves the stones warmer and the shallows clear. High tide at Whitstable can put the sea wall under modest surge during sustained northerly or northwesterly storms; the storm of 1953 flooded the town centre and the flood levels are still marked on some older buildings. Windsurfers and kitesurfers use the beach west of the harbour. The estuary gives a consistent westerly in afternoon sea breeze conditions, with enough fetch across the Thames Estuary to generate proper chop. The tidal range matters for launching: at low water the shore is very shallow for a long run, and returning to the beach at low water can require carrying gear over 200 metres of wet shingle. The Whitstable to Seasalter stretch west of town is one of the better walks on the north Kent coast. Low water reveals the stony foreshore and the remains of old oyster tanks. Waders — dunlin, grey plover, turnstone — feed along the tide line. Photographers get dramatic light on autumn evenings when the sun sets over the estuary. Tide predictions on this page come from Open-Meteo Marine, a gridded global ocean model, cross-referenced with UK Environment Agency gauge data. For the most accurate local predictions, consult the UK National Tide Gauge Network via CEFAS or the UKHO's EasyTide service.