Rostock 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/Berlin local. Folk tradition, not a scientific forecast.

Rostock sits at the mouth of the Warnow river on the Mecklenburg coast, its seaside district of Warnemünde facing north directly into the Baltic Sea. Anyone arriving here from the German North Sea coast — from Sylt or Cuxhaven, where the tide runs 3 to 4 metres on springs — encounters something that requires a complete mental reset. The astronomical tidal range at Rostock is less than 0.3 metres. In practical terms the moon and sun do not move the water here in any meaningful way. The Baltic Sea is a nearly enclosed basin connected to the North Atlantic only through the narrow, shallow Danish straits — the Oresund, the Great Belt, and the Little Belt — and the tidal signal is almost entirely suppressed by the basin geometry before it gets anywhere near Mecklenburg. What moves the water at Warnemünde is the wind. A sustained northeast wind pushing down from Scandinavia — the Nordostwind — drives a wind setup that can raise water levels 1.0 to 1.5 metres above mean along exposed Baltic shores. These Windstau events are real, they happen multiple times each year, and they are the planning variable that matters here in place of a conventional tide table. The opposite is equally true: a prolonged southwest or westerly wind evacuates water from the western Baltic, pushing levels 0.5 to 0.8 metres below mean. The BSH (Bundesamt für Seeschifffahrt und Hydrographie — the German Federal Maritime and Hydrographic Agency) issues water level forecasts for the German Baltic coast that include the wind-driven setup component. For anyone planning a sailing departure from Rostock Überseehafen, a kayak launch at Warnemünde, or a kitesurfing session on the Fischland shore, the BSH coastal water level forecast is more useful than the tide times on this page. Warnemünde itself is a proper seaside resort by German standards — a wide north-facing sand beach backed by the classic Bäderarchitektur of white-painted gabled houses, a working fishing harbour at the river mouth, the lighthouse tower visible from the beach promenade, and a direct S-Bahn rail connection running through Rostock city to the regional rail network. In summer the beach fills with Berliners, and the Strandbad infrastructure — beach chairs, kiosk, volleyball nets — runs at full capacity. The Rostock port complex to the south handles the major Baltic ferry routes: TT-Line to Trelleborg in Sweden and to Helsinki via the Baltic, Stena Line also serving Trelleborg. These are significant vessels on a significant crossing, and the port channels carry real maritime traffic through the Warnow approach. The Fischland-Darß-Zingst peninsula east of Warnemünde is the defining natural landmark of this coast — a narrow spit of pine forest and dune, almost car-free, with the open Baltic on its northern face and the Bodden lagoon system to the south. The Bodden is the characteristic landscape feature of the western Pomeranian coast: shallow, partly enclosed lagoons behind the barrier islands and spits, connected to the open sea through restricted channels that modulate whatever small tidal or wind-setup signal reaches them. Water levels in the Bodden respond to wind setup even more markedly than the open coast because the restricted connections mean wind-driven water piles up and cannot escape quickly. Prerow and Zingst, on the Darß peninsula, are the primary kitesurf and windsurf locations for this coast — the consistent Baltic sea breeze in summer and the strong autumnal NE wind events make this a committed wind-sports destination. The near-atidal character is actually an advantage for wind sports: there are no tide-dependent launch windows, no significant tidal current in the water, and the Bodden lagoon provides a flat-water option when the open Baltic is rough. For sailors, the lack of tide means anchoring and mooring decisions are not dominated by tidal stream and range calculations — but the wind-setup water level variations mean depth readings on charts can be significantly off during sustained wind events. Always apply the BSH forecast correction when working shallows in the Bodden or approaching the Darß shore. Anglers fishing the Warnemünde groyne tips and the rocky training walls at the harbour mouth target sea trout (Meerforelle) and herring — the sea trout run in autumn is the principal seasonal event on the southern Baltic coast, with fish moving into river mouths including the Warnow from September through November. The tide predictions shown on this page come from Open-Meteo Marine, a global gridded ocean model — model-derived, not from a local gauge, and typically accurate within plus or minus 45 minutes on timing and 0.2 to 0.3 metres on height. At Rostock, the predicted tidal variation is so small (under 0.3 metres) that wind-driven water level changes will frequently exceed the entire astronomical tidal range. Monitor BSH coastal water level forecasts alongside any tide-time information here.