Varadero 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 04:00 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 America/Havana local. Folk tradition, not a scientific forecast.

Next spring tide on Fri 01 May (range 0.6m). Last neap on Wed 29 Apr. Next neap on Tue 05 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.

Varadero occupies the Hicacos peninsula, the long thin sandy spit that projects northeast from the Cuban mainland into the Atlantic east of Matanzas city. The peninsula is twenty-two kilometres long and rarely more than 1.2 kilometres wide; the entire northern shore is one continuous sandy beach exposed to Atlantic swell wrapping in from the northeast, while the southern shore, facing the shallow Cárdenas Bay, is sheltered, mangrove-lined and tidally calmer. The tide here is mixed semidiurnal and modest. Mean astronomical range along the Atlantic side runs roughly 30 to 50 cm — slightly larger than the figure inside Bahía de la Habana because the peninsula projects into open water and picks up a fuller tidal signal than the harbour reach in the capital. Two unequal highs and two unequal lows each day, with the diurnal inequality producing one stronger high and one weaker high in most lunar phases. The slope on the Atlantic-side beach is gentle, and the visible width of dry sand changes by several metres between high and low water on a spring tide; on the largest spring lows around new and full moons the wide flat exposes pockets of shell, sea glass and the occasional turtle track in the early morning. The Hicacos peninsula was, until the early twentieth century, partly cut off from the mainland by a tidal channel at its base; the modern Vía Blanca road crosses the lagoon connection on a low causeway, and the channel current there reverses with the tide, slack and gentle most of the year and noticeably stronger only on spring ebbs combined with a Cárdenas Bay drainage event after heavy rain. The dominant non-astronomical driver of water level is weather. Winter cold fronts (frentes fríos) push elevated water along the northern shore and produce a steeper, choppier swell regime; summer easterly trade-wind setup is the more typical warm-season pattern, generally benign. Tropical-system threats peak in August through October; named storms produce surge that exceeds the entire astronomical range many times over. Snorkellers and divers work the inshore reef ledges, the Saturno cave system inland of the resort strip — a freshwater cenote dropping to clear blue depth in a karst sinkhole — and the offshore wrecks accessible by boat from the marinas at Marina Gaviota and Marina Chapelín. The Cueva de Ambrosio in the Varahicacos Ecological Reserve at the northeastern end of the peninsula holds Taino pictographs and is accessible from the same trail network that leads to the Punta Hicacos lighthouse and the wild northeastern beaches beyond the resort strip. Shore anglers cast from the rocky points at the western base of the peninsula and from the Punta Hicacos lighthouse rocks at the northeastern tip for jack, snapper and the occasional bonefish on the Cárdenas Bay flats behind the peninsula. Paddlers launching from the lagoon side find a sheltered regime through the mangrove channels; paddlers on the Atlantic side plan around swell and trade-wind direction. Beach-walking families along the resort strip benefit from the predictable shallow slope and the moderate tide; the wide flat sandy stretch between the resorts and the water line at Cuarta Avenida exposes about 10 to 15 metres of additional dry sand on a spring low, useful for early-morning walks and shell collecting. Photographers favour the early morning low for the wide pristine sand and the low-angle Atlantic light, and the late afternoon high for the foreshortened beach and the warm sky behind the casuarina pines. Kite-surfers find the consistent easterly trade window from late spring through early autumn the best season; the lagoon side at the western base of the peninsula offers a flat-water entry. The authoritative tidal reference for Cuban waters is the Instituto Cubano de Hidrografía (GEOCUBA), which publishes harmonic predictions for the principal Cuban ports. NOAA's Key West gauge provides a useful regional cross-reference for the Florida Straits and Atlantic-side Cuba regime once the local offset is applied. 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 — at Varadero, where the full astronomical range is 30 to 50 cm, the timing uncertainty is a meaningful fraction of the half-cycle and the height uncertainty is a meaningful fraction of the total swing. Treat the predicted highs and lows as approximate. For activity-critical timing, weight GEOCUBA's authoritative predictions and the swell and wind forecast issued by the Instituto de Meteorología de Cuba.