De Haan 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 06:00 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/Brussels local. Folk tradition, not a scientific forecast.

Last spring tide on Tue 19 May (range 4.4m). Next neap on Sat 23 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.

De Haan sits roughly midway along Belgium's 67 km North Sea coast, a resort town that looks unlike any other on this stretch because of a building restriction put in place more than a century ago: no high-rise construction was permitted, and the policy held. The result is a town of Belle Époque villas, art nouveau guesthouses, and turreted seaside architecture from the 1890s to 1930s preserved inside the curved street plan laid out by the original developers. Where Ostend 10 km to the southwest has a casino promenade and De Panne to the west has waterpark infrastructure, De Haan retained the low-density, tree-shaded character of its origins. The Belgian coast tram — the Kusttram — runs the full 68 km from De Panne to Knokke-Heist, reputedly the longest tramline in the world, and De Haan sits on it. The journey to Ostend takes 20 minutes. The tide at De Haan is a genuine North Sea semidiurnal tide, and the range is large relative to most European Atlantic coasts. Mean spring range runs 4.0 to 5.0 m. That is enough to expose several hundred metres of tidal flat at low water — the beach at De Haan is wide at low tide and narrow at high, and the difference between the two is dramatic. The tidal flat exposed at low water stretches 300 m or more from the dune foot, revealing ridged sand, runnels, and shell debris. On a neap low the flat is smaller; on a spring low the expanse of wet sand runs to the horizon. Children with nets and buckets have productive hours at the low-water mark; shore anglers casting from the beach for flatfish and bass find the flood tide the traditional window as the returning water pushes baitfish over the sand. The dune system behind the beach is part of a protected coastal dune landscape (Duinen en Polders) that extends along much of the Belgian coast. At De Haan the dunes are active — mobile crests 8 to 12 m high immediately behind the beach — and the vegetation succession from bare sand to fixed dune to dune slack to woodland is readable on a 10-minute walk back from the high-water mark. The dune slack ponds hold natterjack toad populations and are closed to access in the breeding season. The flood tide at De Haan runs for approximately 6 hours; the ebb runs slightly longer due to the shallow shelf geometry. The tidal current along the beach is directed roughly northeast on the flood and southwest on the ebb, and longshore drift is active — the groynes visible from the beach are managing sand transport that would otherwise redistribute the beach southwestward. Kite-buggy and kite-surfing sessions run from the beach at low water when the flat is exposed and the wind is in the southwest to northwest, which is the dominant quadrant on this coast. Predictions on this page come from Open-Meteo Marine, a gridded global ocean model. Accuracy is typically within plus or minus 45 minutes on timing and 0.2 to 0.3 m on height — at De Haan's spring range of 4.0 to 5.0 m, the height uncertainty is a small fraction of the total swing, so the predictions are more useful here than at microtidal stations. For activity-critical timing, the Belgian coast tide tables published by the Vlaamse Hydrografie (within the Flemish government's Departement Mobiliteit en Openbare Werken) provide the authoritative harmonic predictions for Oostende, which is the reference port for this stretch of coast. De Haan's actual high-water time is typically within a few minutes of Oostende's.