Jeffrey's Bay 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 06:00 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/Johannesburg local. Folk tradition, not a scientific forecast.

Last spring tide on Thu 07 May (range 0.8m). Next spring tide on Wed 13 May (range 1.2m). Next neap on Sat 09 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.

Jeffrey's Bay is 75 kilometres southwest of Gqeberha, a small town of 30,000 that exists in the global surf imagination at a scale entirely disproportionate to its size. The right-hand point break here — specifically the Supertubes section, where the groundswell wraps around the point and refracts along the sandy bottom to produce long, fast, almond-shaped walls — is consistently rated among the five best point breaks in the world. The WSL (World Surf League) Rip Curl Pro at Jeffrey's Bay has been the centrepiece of the Championship Tour since 1984 and is the contest most professional surfers most want to win. Tidal range at J-Bay is approximately 1.6 metres mean above Chart Datum — semidiurnal, close to but slightly smaller than the Gqeberha figure, with the characteristic two-high two-low daily rhythm of the South African east coast. The tide state is one of the operative variables for the quality of the break. Supertubes performs best at mid-tide, when there is sufficient water over the sand shelf for the wave to pitch and peel cleanly. At full high water the break often loses definition — the wave becomes fat and crumbles rather than throwing — and can close out across the section. At low tide, particularly on larger south groundswell, the bottom is shallow enough to create hazardous sections. The mid-tide window is the session window at J-Bay: the difference between a 5-second and a 40-second ride can be a matter of half a metre of water. The swell that drives J-Bay is long-period south and southwest groundswell generated by Southern Ocean storms in the Roaring Forties and Fifties. The fetch is unobstructed from the Antarctic convergence zone, and the groundswell that arrives at J-Bay has travelled thousands of kilometres in organised pulses, which is why the waves here are long and clean rather than windswept and chaotic. South swells — more directly perpendicular to the point's angle — typically produce longer rides than southwest swells, which can be more powerful but sometimes race through the sections too fast. Beyond Supertubes, the J-Bay break has multiple sections: Kitchen Windows, Boneyards, Supertubes, Impossibles, Tubes. Each has its own character and responds differently to swell direction and size. Kitchen Windows is the most accessible for intermediate surfers on smaller days. The Main Beach and Point sections handle the learning and longboard crowd. On the rare big days when south groundswell tops 3 metres and all sections connect, the break produces one of the longest rideable waves on the planet — rides of over a minute have been documented in contest footage. The town around the break is small and entirely oriented to surf tourism. Accommodation ranges from backpacker hostels to high-end point-facing guesthouses. The WSL contest window is July, when south groundswell frequency and size is at annual maximum and the water temperature drops to around 16°C — a full wetsuit is standard. Summer (December–February) produces smaller but more consistent swell with 19–21°C water. Spring (October–November) is often cited as the best balance of swell, crowd level, and water temperature. 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 metres on height — model-derived, not from a local gauge. For authoritative South African tide data, consult SANHO (South African Navy Hydrographic Office), which publishes official tide tables for Eastern Cape stations.