Nadi Coast 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 10:00 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 Pacific/Fiji local. Folk tradition, not a scientific forecast.

Next spring tide on Wed 13 May (range 1.4m). 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.

The Nadi coastal strip is the entry point for the majority of international visitors to Fiji. Nadi International Airport, on the flat coastal plain of the Viti Levu western coast, is the primary gateway for flights from Australia, New Zealand, Asia, and North America. The Denarau resort complex a few kilometres to the west is where most visitors spend their first and last nights, and Port Denarau marina is the departure terminal for ferries and catamarans to the Mamanuca Islands, the Yasawa Islands, and the various resort islands in the western Fiji group. Denarau Island is a purpose-built resort and marina precinct created on reclaimed land, connected to the Viti Levu mainland by a short causeway. The marina's dredged channel approach is tide-insensitive at the ferry berth level: the channel maintains navigable depth across the full tidal range for the catamarans and larger ferry vessels used on the island routes. The resort hotels on Denarau range from mid-market to international chain properties; the strip along the beach-facing side of the peninsula has beach club and pool infrastructure, but the beach itself is not the main draw — the offshore islands are. The tidal regime along the Nadi coast is mixed semidiurnal. Spring range at nearby Lautoka, the main coastal reference point 23 km north, runs approximately 1.2 to 1.5 m. Two highs and two lows per day with measurable diurnal inequality — the higher high and the lower high in a given day can differ by 0.3 to 0.5 m on the most unequal days. The spring-neap variation across the lunar month modulates the range, with the largest spring tides around new and full moons. The beaches immediately adjacent to Nadi and Denarau are not the primary swimming beaches in the area. Water clarity around the Nadi River mouth and the coastal zone behind Denarau is affected by river silt and tidal flat sediment from the extensive mangrove systems that fringe this coast. The reclamation for Denarau Island replaced mangrove wetland, and the sediment transport patterns in the tidal zone behind the causeway reflect that history. Visitors looking for beach swimming use the Mamanuca Island transfers from Port Denarau rather than the Nadi mainland coast. For anglers and kayakers, the tidal flat zone behind Denarau and through the inshore mangrove channels offers worthwhile estuary-species fishing — mangrove jack, bonefish on the exposed flats at low water, and barramundi in the creek mouths. The flat between the causeway and the mangrove fringe exposes at low water on spring tides; the productive window for flat walking or kayaking into the mangrove is the two hours either side of the predicted low. A guide familiar with the local channels is useful — the mangrove maze around the Nadi estuary is extensive and the channels look similar throughout. The Sabeto mountain range immediately behind Nadi creates an orographic rainfall pattern: the Nadi area receives more rain than the drier western Viti Levu coast further south, and the Nadi River rises quickly after heavy rain, adding turbid water to the coastal zone for a day or two following significant rainfall events. The Coral Coast, along the southern Viti Levu shore accessible by the Queen's Highway from Nadi, offers a different beach character from the resort islands: fringing reef close to shore, village communities along the road, and calmer water in the lagoon inside the reef. The Pacific Harbour and Sigatoka areas on the Coral Coast are within 60 to 90 minutes' drive of Nadi airport and offer an alternative for visitors with limited time who want a mainland beach rather than an island transfer. 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 m on height. The Fiji Meteorological Service publishes authoritative marine and weather forecasts for Fijian waters.