Las Palmas de Gran Canaria 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 1.8m). 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.

Las Palmas de Gran Canaria sits on the northeast corner of Gran Canaria, a volcanic island 100 kilometres off the coast of southern Morocco, roughly level with the Western Sahara. It is the largest city in the Canary Islands and one of the most important Atlantic port cities in Europe — Puerto de la Luz, the city's commercial harbour, handles a significant share of the container, cruise, and fishing traffic transiting the central Atlantic route between Europe and South America. The city's geography organises itself around two distinct coastal faces: the port and old quarter (Vegueta, Triana) on the sheltered western side, and the city beach on the northeast. Playa de Las Canteras is the defining urban beach — 3 kilometres of sand running along the northeast face of the Isthmus of Guanarteme, protected on its seaward side by La Barra, a natural submerged reef that parallels the beach 50 to 200 metres offshore and breaks the Atlantic swell before it reaches the sand. Inside La Barra the water is calm enough for year-round open-water swimming; outside the reef, the Atlantic swell runs unimpeded from the open ocean. The northern end of Las Canteras (the Punta del Confital area) is exposed and takes bigger swell — a surf break that works on northwesterly Atlantic groundswells. The southern end, inside the main reef protection, is where families and lap swimmers operate year-round. The tide at Las Palmas is semidiurnal Atlantic, with a mean range of approximately 1.5 to 2.0 metres. Spring tides push the swing toward 2.5 metres; neap tides reduce it to around 1 to 1.2 metres. Two highs and two lows per day, with a modest diurnal inequality — the Canary Islands sit at 28 degrees north, where the mixed semidiurnal pattern is fully established and the difference between the two daily highs is usually 10 to 20 centimetres. That range is enough to alter the character of Las Canteras at different states of the tide: at low water, sand flats inside La Barra expose rocky sections of the reef shelf and the beach widens considerably; at high tide, the reef is covered and the narrow inner channel behind La Barra runs faster as the tidal prism floods and ebbs through the gaps in the rock. The trade wind — the northeast Alisio — is the dominant environmental feature of the Canary Islands, blowing with high consistency most of the year. The eastern islands of Fuerteventura and Lanzarote sit closer to the African continent and receive the strongest and most uninterrupted trade wind flow; Fuerteventura's surf and kite coast around Sotavento and La Pared is one of the world's fixed points for professional windsurfing competition. Gran Canaria receives a more moderated trade wind, partly deflected by the island's volcanic profile (the peak of Pozo de las Nieves reaches 1949 metres). The northern coastal area around Las Palmas is more wind-exposed than the sheltered southwestern coast, which lies in the island's wind shadow and is warmer and calmer but offers fewer water-sport conditions. From an angling perspective, the Atlantic waters off Gran Canaria are deep — the island sits on the edge of the Canary Bank and the ocean floor drops steeply within a few kilometres of the coast. Bluefin tuna, marlin, and wahoo transit these waters, and the sport-fishing fleet out of Puerto de la Luz is active year-round. Reef fishing inside the protected marine reserve areas around the coast requires awareness of current boundaries that shift with the tidal state and wind setup. Swimmers and snorkelers using Las Canteras time their sessions for the rising tide, when the incoming flood pushes clearer Atlantic water through the reef gaps and visibility inside La Barra is best. At low tide, the sand on the reef shelf can be stirred by wave action across the exposed rock sections, and visibility inside the protected area drops. The Columbus House museum (Casa de Colón) in the Vegueta historic quarter documents the Atlantic trade route context — Cadiz and Las Palmas were the last European ports on the outward voyage to the Americas for most of the colonial period, and the city's Atlantic position is not incidental to its history. 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 a local gauge. Puertos del Estado operates the Las Palmas gauge and publishes official tide data; the Instituto Hidrográfico de la Marina covers the Canary Islands in the Spanish tide almanac.