Ada Foah 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 22:00 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 Africa/Accra local. Folk tradition, not a scientific forecast.

Last spring tide on Wed 20 May (range 1.4m). Next neap on Sun 24 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.

Ada Foah is at the mouth of the Volta River, where West Africa's largest reservoir system finally meets the Atlantic. The river mouth here is not a single defined channel but a shifting delta of sand spits, tidal creeks, and lagoon inlets — a hydraulic junction that produces some of the most complex water conditions on the Ghana coast. On one side of the narrow sand spit is the river; on the other, the Atlantic surf. Both are accessible from the cluster of eco-resorts and lodges that have made Ada Foah one of Ghana's most visited beach destinations. Tide data for Ada Foah uses Open-Meteo Marine, a global gridded ocean model. Accuracy for this stretch of the Gulf of Guinea coast is typically ±45 minutes on timing and ±0.2 to 0.3 metres on height. The tidal pattern is semidiurnal with a spring range of 0.8 to 1.2 metres — a moderate range by West African standards, with the Gulf of Guinea tending toward the lower end of the West African scale. Wind effects and the Volta's discharge add significant variability on top of the astronomical tide. The Volta River discharge is the defining variable at Ada Foah. The Akosombo Dam, completed in 1965, fundamentally changed the river's behaviour: before the dam, seasonal flood pulses from the Volta basin reached the river mouth and deposited sand, maintaining the delta spits. Post-dam, reduced sediment load has accelerated coastal erosion, and the river mouth has migrated multiple times. The sand spit that currently separates the river lagoon from the Atlantic is narrower and less stable than it was in the mid-20th century. For beach users, the Atlantic face of the sand spit at Ada has persistent surf. Tide stage affects the wave character: at low tide the beach gradient steepens and waves dump on the foreshore. At high tide the beach is wider and the waves break further offshore, making conditions gentler for swimming. The river lagoon side is calm and shallow — ideal for kayaking and SUP. Most resorts keep a fleet of canoes and kayaks for guest use. For anglers, the river mouth zone is highly productive on the outgoing tide. The current flush pushes bait and small fish through the mouth, concentrating predators: ladyfish, barracuda, African moonfish, and the locally prized African threadfin (capitaine) are all caught in this zone. Charter boats operating from the resort jetties run trolling and casting trips into the mouth zone from first light. Shore casting from the river banks is also productive. Kayaking from Ada Foah into the river delta system is a full-day activity: the network of creeks and lagoon arms extends for several kilometres upstream, with mangrove corridors, fishing villages accessible only by water, and occasional monitor lizard sightings on the banks. Tide planning for these trips matters: entering the creek system on a rising tide and returning on the ebb uses the current efficiently. Water temperature here runs 26 to 29°C for most of the year, with a cold upwelling period from June through August when Atlantic surface temperatures can drop to 22 to 24°C offshore. The resort infrastructure at Ada Foah has grown significantly since the early 2000s. Several eco-resort properties operate on the lagoon (river) side of the spit, offering kayak hire, boat excursions, and guided river trips. The standard day-trip format from Accra — 100 kilometres west on the Accra–Tema motorway and then south on the Sogakope road — has made Ada Foah Ghana's most accessible beach and river destination from the capital. Journey time from Accra is approximately 2 hours by private vehicle. The river mouth zone at Ada Foah is a productive site for observing the interaction between fresh and salt water. On clear days, the colour boundary between the brown Volta water and the blue-green Atlantic is visible from the beach. The mixing zone shifts with tide stage: on the incoming tide, the saltwater wedge pushes upstream under the lighter freshwater; on the ebb, the freshwater layer rides over the denser salt water as it moves toward the sea. This stratification is a significant factor in the ecology of the estuary — juvenile fish use the salinity gradient as a habitat indicator, and adult fish time their movements across the boundary with the tidal cycle. The Ada Foah Yacht Club and the Ada Estuary Hotel, both on the lagoon side, are the established social and water-sports hubs. Kitesurfing has become a notable activity in the lagoon during the harmattan season (November to February), when the northeast trade wind blows consistently at 15 to 25 knots across the lagoon surface.