Santander 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/Madrid local. Folk tradition, not a scientific forecast.

Last spring tide on Sat 02 May (range 3.1m). Next neap on Fri 08 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.

Santander sits at the mouth of a large ría — a drowned river valley carved by Pleistocene glaciation and now drowned by post-glacial sea level rise — on the southern shore of the Bay of Biscay. The bay itself is a broad semicircular body of water almost 50 kilometres across at its widest, open to the ocean to the north and sheltered by the mountainous Cantabrian coast to the south. The tidal range here is 3.5 to 4.0 metres, semidiurnal, making it one of the largest tide regimes on the Spanish coast and a sharp contrast to the negligible tides of the Mediterranean Spain that most visitors picture. Spring tides around new and full moons routinely exceed 4 metres at Santander; neap tides drop back toward 2 to 2.5 metres. The city occupies the northern shore of the ría, looking across the water to the Somo and Loredo beaches on the southern spit. El Sardinero, on the exposed Atlantic side of the peninsula northeast of the city centre, is the city's famous beach — a wide, gently curved strand exposed to the Bay of Biscay swell that has been the summer destination for the Spanish royal family and Madrid's upper class since the early 20th century. The Palacio de la Magdalena, the royal summer palace completed in 1912 and donated to the city by the people of Santander in 1941, sits on the headland at the eastern end of El Sardinero. At low tide, El Sardinero is a wide, firm, family-scale beach. At high tide, the waves run close to the seawall. Two kilometres south of El Sardinero, across the narrow water at the bay entrance, Playa de El Puntal is the sandspit beach that runs along the southern shore of the bay mouth. El Puntal is one of the most tide-dependent beaches on the Cantabrian coast. There is no road to it. At high tide, the water around the spit is several metres deep and the only access is the small passenger boat (El Puntal ferry) that runs from the Embarcadero de Pereda in central Santander during the summer season. As the tide falls, the sandflat on the bay side of the spit progressively dries and, by the time the tide is within 90 minutes of its predicted low, it is possible to wade across from the Somo beach. By low water, the connection is firm sand. The timing matters: anyone planning to walk to El Puntal from Somo needs to check the tide table in advance, because the window between accessible and stranded is only a few hours. The Somo beach itself, across the bay from the city, is the surf coast. A semidiurnal tide of 3.5 to 4.0 metres means the surf break character changes completely between high and low tide — the bank that works at half tide may be closed out at high and dry at low, and the paddle from the beach to the break is substantially longer on the ebb. The Cantabrian surf community has been riding these waves since the 1970s and the local knowledge about which breaks work on which tide state is detailed. The Atlantic swell pattern along the Cantabrian coast is strongest through autumn and winter, when frontal systems tracking across the North Atlantic send west and northwest groundswell into the Bay of Biscay. The Picos de Europa, visible on the southern skyline from Santander on a clear day, catch the same Atlantic weather systems that drive the swell. The bay estuary itself holds a rich ecosystem — the intertidal flats exposed on the ebb are feeding habitat for wading birds, and the channels hold sea bass that move with the tidal current. Anglers working the bay target the tide-driven feeding patterns along the channel edges and the sea walls at the bay mouth. The 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 metres on height — model-derived, not from the Santander gauge. Puertos del Estado operates the Santander sea-level station, one of the longest and most complete tide records on the northern Spanish coast. The Instituto Hidrográfico de la Marina publishes the official Spanish tide almanac covering the Bay of Biscay.