Port Moresby 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 09:00 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/Port Moresby local. Folk tradition, not a scientific forecast.

Next spring tide on Sat 16 May (range 2.2m). Last neap on Wed 13 May. Next neap on Tue 19 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.

Port Moresby is the capital of Papua New Guinea, positioned on a peninsula of raised coral limestone at the head of Fairfax Harbour on the Coral Sea coast. The city of roughly 400,000 is the largest in the Pacific island region outside Australia and New Zealand. Two natural harbours — Fairfax Harbour to the north and Bootless Bay 12 kilometres to the east — frame the city's coastal access, and the inner harbour has been central to PNG's trade since the colonial period. The tidal regime at Port Moresby is semidiurnal with a spring range of approximately 2.0 m. Two daily tidal cycles of broadly similar height drive a moderate tidal current through the Basilisk Passage — the main navigable entrance to Fairfax Harbour between the mainland and the reef system to the south. The Papuan Barrier Reef runs along this coast 20–30 kilometres offshore, sheltering the coastal waters from open Coral Sea swell and creating a shallow inner sea between the reef and the mainland coast. This inner sea, 1–5 m deep over its central sections, is an extensive intertidal and sub-tidal habitat that is among the least disturbed in the world. The reefs along the Papuan Barrier Reef are rarely dived — access requires a boat capable of the 20–30 km offshore transit. Ela Beach is the main urban beach, a 200-metre crescent of sand 2 kilometres southeast of the city centre, adjacent to the Ela Beach Hotel and the Port Moresby Sailing Club. At high spring water the beach narrows to 15–20 metres and the Coral Sea swell arrives directly at the sand; at low spring water the beach widens to 40–50 metres and the reef flat offshore is exposed. The reef immediately south of Ela Beach provides snorkelling at mid-tide and above — coral coverage is moderate given the beach's proximity to the city, but fish diversity is higher than the urban location might suggest. Visibility is 5–12 m close to shore; it improves sharply at the Basilisk Passage mouth where Coral Sea water exchanges with harbour water. Bootless Bay, 12 km east of the city centre, is the primary recreational marine hub. The bay is enclosed by a reef and headlands that moderate the swell, and several reef dive sites are accessible within 10–15 minutes by boat from the Bootless Bay Marina. The Suzie, Peligrade Point, and Sinub Island sites are within recreational diving range (15–30 m depth) and are accessible at any tidal state, though dive operators time their drops to the slack-water window around high and low tide when current over the reef is minimal. The bay's mangrove margins, accessible by kayak on the upper tidal stages, hold herons, kingfishers, and the variable mudskipper community typical of tropical mangrove coasts. The fishing from Port Moresby is substantial. The inner coastal waters between the city and the Papuan Barrier Reef support a commercial and recreational fishery for reef species — snapper, coral trout, and emperor — that are lightly exploited relative to the size of the reef system. Offshore beyond the barrier reef, the blue-water fishery produces yellowfin tuna, wahoo, and black marlin. Black marlin weighing over 300 kg are taken regularly in the waters offshore of Port Moresby between October and April, a season driven by the marlin migration through the Coral Sea. The annual Port Moresby game-fishing competition is one of the Pacific's longest-running events. For families, Ela Beach and the calmer sections of Bootless Bay are the primary swimming locations. Sea temperature is 26–29°C throughout the year. The November–April wet season brings the possibility of rough conditions from tropical weather systems; May through October is the southeast trade-wind season, when conditions are more predictable and the sea state is generally more settled. For photographers, the Port Moresby Harbour at sunrise — with the traditional lagatoi trading canoes (double-outrigger sailing canoes with crab-claw sails) occasionally visible during the Hiri Moale festival season — and the Ela Beach sunset are the primary coastal subjects. The reefs visible through the Basilisk Passage at low water, with the barrier reef visible on the horizon, give a sense of the scale of the reef system that frames the city. All tide predictions for Port Moresby come from the Open-Meteo Marine gridded model. Timing accuracy is ±45 minutes; height accuracy is ±0.3 m above Chart Datum.