Haapsalu 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 07:00 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/Tallinn local. Folk tradition, not a scientific forecast.

Haapsalu is a spa town on the western coast of mainland Estonia, where a shallow bay — the Haapsalu laht — reaches inland through a complex of reed beds, mudflats, and small islets backed by pine forest. The town itself is built on a low limestone peninsula that projects into the bay, with the ruins of the Bishop's Castle of Haapsalu (13th century, partially restored) anchoring the historic centre and the long wooden promenade along the bay — the Kuursaal promenade — stretching from the railway station pavilion to the park at its eastern end. The railway pavilion, built in 1905 for Tsar Nicholas II's arrival by the imperial train, is the longest railway platform in the Baltic States: 216 m. The African Beach (Aafrika rand), as it has been called since the 1920s, is the shallow, sheltered swimming beach on the eastern side of the bay, popular for its warm, relatively clear water — the bay is shallow enough that it heats significantly in summer, reaching 24 to 26°C in July, warmer than many Baltic open-coast beaches. The name is an ironic reference to the warmth relative to the rest of Estonia's coast. The White Lady of Haapsalu Castle is a local legend: a ghost said to appear in the castle's window during the full moon in August, a tradition maintained by a projection and theatrical performance staged for August visitors. The projection itself dates from the Soviet period; the castle ruin is genuine 13th-century German Order architecture. The Baltic tidal regime at Haapsalu is genuinely microtidal: mean astronomical range 0.1 to 0.3 m. As throughout the Baltic, the tidal signal is marginal and dominated by wind-driven water-level changes. The bay at Haapsalu is particularly shallow — depths rarely exceed 2 to 3 m in the inner bay — and wind-driven water-level changes of 0.5 to 1.0 m are common during Baltic storm events. A sustained westerly wind piles water into the bay; an easterly drains it. This seiching character means that on stormy days the bay level fluctuates in ways that have nothing to do with the moon. The shallow water also creates a sensitive response to ice conditions: the bay typically freezes in January and February, with the ice cover reaching 20 to 40 cm in cold winters. Ice walking and cross-country skiing across the frozen bay to the offshore islands is a local winter tradition. The therapeutic mud (sapropel) harvested from the bay bottom has been used at Haapsalu's sanatorium since the early nineteenth century. The spa tradition here is real and active: several hotels and a dedicated treatment centre offer mud therapy for musculoskeletal conditions, and Haapsalu was one of the main spa destinations for the Russian aristocracy and St Petersburg intelligentsia before 1914. Predictions on this page come from Open-Meteo Marine, a gridded global ocean model. At Haapsalu's 0.1 to 0.3 m astronomical range, the model's typical accuracy (plus or minus 45 minutes, 0.2 to 0.3 m) equals the full signal. For actual water-level conditions, the Estonian Environment Agency (Keskkonnaamet) and the Tallinn University of Technology operate bay-level monitoring that is more informative than the astronomical tide prediction for any activity dependent on precise water level in the Haapsalu laht.