Baconao 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 00:00 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 Sun 17 May (range 0.5m). Last neap on Fri 15 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.

Baconao extends along the south coast of Santiago de Cuba province east of the city, from the Río Baconao mouth to Punta Caleta, a stretch of roughly 30 km of coast designated as the Parque Baconao — a UNESCO Biosphere Reserve since 1987. The terrain here differs from the dramatic cliffs of the Chivirico section to the west: low hills covered in dry tropical scrub back the coast, with sandy beaches interrupted by rocky headlands and a scatter of small rivers running down from the interior. The Caribbean exposure is direct — this coast faces south and southeast without significant offshore shelter, making it more exposed to open Caribbean swell than the inner harbour of Santiago or the cliff-shielded anchorages of the Chivirico section. The tidal regime is mixed semidiurnal Caribbean microtidal. Mean spring range on this south-facing open coast runs roughly 30 to 50 cm, with the same two-unequal-highs, two-unequal-lows daily pattern characteristic of the mixed Caribbean tide. The diurnal inequality produces one stronger daily high and one weaker high; on neap tides the swing compresses to 15 to 25 cm. Weather drivers — Caribbean swell from the southeast, the Windward Passage wind regime, and occasional tropical disturbance — produce water-level changes that frequently exceed the astronomical signal. The Instituto Cubano de Hidrografía (GEOCUBA) is the authoritative tidal reference; predictions on this page come from Open-Meteo Marine, a gridded global ocean model, accurate to approximately ±45 min and ±0.2–0.3 m. The Valle de la Prehistoria, roughly 2 km inland from the coast at the Baconao reserve, is an open-air sculpture park of 227 life-size concrete dinosaurs and prehistoric humans, built by Cuban military recruits in the 1980s across a hillside of low scrub. It is the most-visited single attraction in the reserve and a useful orientation point for the coast road east of Santiago city. The park itself sits at about 80 m elevation; on a clear day the overlook behind the main entrance has a view southwest over the dry hill country toward the coast. For beach access, the reserve encompasses several beaches accessible from the coast road (the Vía Baconao, which runs east from Santiago city through Siboney toward the reserve). Playa Siboney, roughly 15 km from Santiago, is the most established beach in the area — a working fishing village with a small beach used by Santiago residents for weekend visits. Playa Cazonal and Playa Baconao further east are quieter. The beach slope at Baconao is moderate to steep compared to the gentle Atlantic-slope beaches of northern Cuba; the south-Caribbean exposure means the swell approach varies more with Caribbean weather patterns than with the tide. For snorkellers and divers, the rocky headlands between the sandy beach sections hold patch reef communities at shallow depth. Visibility on the open-Caribbean-facing headlands depends on sea state more than on tide state; the low-current conditions just after the predicted high or low give the clearest window in calm weather. The Biosphere Reserve designation prohibits commercial extraction within the protected zone, so spearfishing and shellfish collection are restricted. Shore anglers work the rocky points between beaches for jack crevalle and snapper on the incoming tide, with the pre-dawn to early morning window the most productive. The mouth of the Río Baconao at the western end of the reserve is a mangrove estuary that holds tarpon, snook, and juvenile fish on the flooding tide; local anglers wade the estuary channels on the early flood, typically two to three hours before the predicted high. Photographers have a coastline that rewards patience. The contrast between the dry, low-scrub hills and the turquoise Caribbean water is strongest in morning light from the east. The beach at Playa Cazonal has a clean sweep of sand with no resort infrastructure in the immediate frame. The Valle de la Prehistoria at dusk, with the low-angle light catching the concrete sculpture surfaces and the dry scrub silhouetted behind them, is an unusual and photogenic subject. Predictions on this page come from Open-Meteo Marine. Accuracy is typically ±45 min and ±0.2–0.3 m. GEOCUBA harmonic predictions are the authoritative source for navigation and activity-critical timing in these waters.