Skagen 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 10:00 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/Copenhagen local. Folk tradition, not a scientific forecast.

Last spring tide on Thu 30 Apr (range 0.3m). Next spring tide on Mon 04 May (range 0.5m). Next neap on Sun 03 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.

Skagen sits at the very tip of Jutland, the thin spit of sand that runs north from Denmark's mainland until it narrows to Grenen — the point where the Skagerrak and the Kattegat meet in a visible line of clashing water. The two seas arrive from different angles and with different wave patterns, and at Grenen the interference is real and observable: two sets of waves converge, intersect, and produce a turbulent ridge that runs along the sandbar for several hundred metres. It is not dramatic by ocean standards, but it is one of the more tangible illustrations of two bodies of water meeting that you can stand next to in northern Europe. The tide at Skagen is small but slightly larger than Copenhagen's inner harbour. The Skagerrak connects to the North Sea and carries a stronger tidal signal than the closed Baltic; mean astronomical range here runs roughly 30 to 50 cm, and on the largest spring tides around new and full moons the swing can approach 70 cm. That is still modest by North Sea standards — Esbjerg on Denmark's North Sea coast reads a mean range over a metre — but it is enough to expose the wide sand flats at Grenen as the water drops and to produce a noticeable current through the Kattegat approaches. Wind and storm surge dominate, here as at Copenhagen. Autumn and winter northwesterly storms off the Skagerrak push water level well above the predicted range; the sandy coast at Skagen is mobile, with Grenen's tip extending further northeast each decade as the longshore drift from west to east continues. Råbjerg Mile, the large inland moving dune east of Skagen, migrated from the coast and has been moving northeastward at roughly 15 metres per year for centuries. Den Tilsandede Kirke (the Buried Church) at Gammel Skagen is the tower of a medieval church that the drifting sand overtook and buried — the tower persists as a local landmark and a record of what the sand drift does over centuries. Skagen Lighthouse on the northwestern peninsula is the primary navigation light for the Skagerrak-Kattegat transition, and the Skagen Fiskeauktion (fish auction) at the harbour is one of Denmark's most active. Shore anglers here work the sandy points for sea trout and flatfish on the changing current; the incoming tide from the Skagerrak side and the early ebb are the traditional windows for the sandy-point casters. DMI (Danmarks Meteorologiske Institut) publishes the authoritative sea-level and surge forecasts for the Danish coast, including the Skagen gauge. Predictions on this page come from Open-Meteo Marine gridded model — useful for identifying the approximate rhythm of high and low, but the uncertainty on timing and height can be a significant fraction of the total signal at this location. Weight DMI's real-time gauge and forecast data for any activity where precise water level matters.