Paracas, Peru 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 23:00 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/Lima local. Folk tradition, not a scientific forecast.

Last spring tide on Mon 18 May (range 1.0m). Next neap on Fri 22 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.

Paracas sits on the northern shore of the peninsula of the same name, 250 km south of Lima on the Pacific coastal desert. The Paracas National Reserve covers the peninsula and the adjacent sea — some 335,000 hectares of protected land and marine territory, encompassing the cold upwelling zone where the Humboldt Current drives one of the most productive marine ecosystems on Earth. The Ballestas Islands, 20 km offshore from El Chaco port, hold approximately 150,000 Humboldt penguins, tens of thousands of Peruvian boobies, fur seal colonies, and dolphin pods that are present year-round on the nutrient-rich cold water. The tidal regime at Paracas is Pacific semidiurnal with a mean range of approximately 1.0 to 1.5 metres — larger than the Caribbean locations, with the tide playing a more significant role in planning activities on the beach and at the reserve access points. Two clearly distinct highs and two lows per day characterize the pattern, with a modest diurnal inequality. The Humboldt Current upwelling periodically creates mesosynoptic sea-level anomalies — the cold water wedging shoreward from offshore can depress coastal sea level by several centimetres over multi-day periods, which appears as an apparent shift in the tide prediction. On longer timescales, El Niño years warm the surface water, suppress the upwelling, and shift the sea level anomaly the other way. The Ballestas Islands are reached by fast zodiac or pangas from El Chaco dock in 30 minutes. The crossing is over open Pacific; sea state depends on the wind and the swell forecast rather than the tide. The tours run standard morning departures (around 07:00–08:00) to catch the birds during their most active feeding period. The sealions on the island rocks are at their most accessible at low tide when the haul-out platforms are fully exposed; a spring low, around 0.2 to 0.3 m above chart datum, extends the visible haul-out surfaces significantly. The tour operators run regardless of tide state, but timing a visit to a morning low tide enhances the sea lion viewing. The Candelabra (Candelabro) geoglyph, carved into the hillside facing the bay north of Paracas, is visible from the boat crossing to the Ballestas — a 180-metre trident-shaped figure whose origin and age are debated (possibly Paracas culture, possibly colonial-era navigation marker). It is not accessible on foot from land. For anglers, the Humboldt Current upwelling drives one of the most productive inshore fisheries in the world. The anchoveta (Engraulis ringens) schools that support the bird and marine mammal populations also underpin the Peruvian artisanal fishmeal and anchovy fishery based at El Chaco. Sport fishing for corvina (Cilus gilberti) is the target inshore; the fish hold in the surf zone and the tidal rip at the rocky headlands on the falling tide, particularly in the two hours before the predicted low water. The El Chaco pier and the rocky points south of the port are the primary shore-casting stations. The beaches of Paracas National Reserve south of El Chaco are accessible by car on the reserve's one road (no public transport inside the reserve; entrance fee required). Playa La Mina and Playa Lagunillas are the main beach stops — both are wide, open Pacific beaches with the cold, clear upwelling water, strong rip currents on windy days, and absolute prohibition on swimming (the reserve prohibits swimming at most of its Pacific beaches due to current and swell hazards). The beaches are for wildlife observation, walking, and photography, not swimming. The dominant atmospheric condition at Paracas is the Paracas wind — a powerful south-to-southwest afternoon wind that builds daily from around 12:00 and can reach 40+ knots by mid-afternoon, driving a veil of sand and dust across the peninsula. Morning activities before 12:00 are calm; afternoon activities on the open peninsula require eye protection and secured equipment. Predictions on this page come from Open-Meteo Marine, a global gridded ocean model. Accuracy is ±45 minutes on timing and ±0.2 to 0.3 metres on height. For the Peruvian coast, the SENAHMI (Servicio Nacional de Meteorología e Hidrología del Perú) and the DHN (Dirección de Hidrografía y Navegación de la Marina de Guerra del Perú) publish authoritative tidal tables.