Osaka 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 13:00 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 Asia/Tokyo local. Folk tradition, not a scientific forecast.

Next spring tide on Sun 03 May (range 1.9m). 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.

Osaka sits at the head of Osaka Bay, the northeastern arm of the Seto Inland Sea, where the Yodo River empties into a shallow coastal plain that the city has been building on and out into for centuries. The bay opens southwest between the tip of the Kii Peninsula and the northern end of Awaji Island, beyond which the Akashi Strait connects it to the wider Seto Inland Sea system. That geometry — an enclosed embayment connected to an enclosed sea — gives Osaka its tidal character: mixed semidiurnal, with two unequal highs and two unequal lows per day, and a mean astronomical range in outer Osaka Bay of roughly 1.5 to 2.0 m. The diurnal inequality is one of the defining features of the tide here. Through most of the lunar month, the two daily highs differ noticeably in height: one dominant high and one secondary high, with a corresponding pair of lows of different magnitude. This is the mixed character of a coast sitting between purely diurnal Pacific forcing and the semidiurnal Atlantic norm, and it means reading the tide chart matters — the 'high' at 6 am and the 'high' at 6 pm may differ by half a metre or more depending on lunar phase. Practical consequences are spread across the coast. The Nanko district in southern Osaka is the most immediately tide-relevant: Sakishima houses the Osaka Aquarium Kaiyukan on an artificial island linked to the mainland, and the waterfront at Nanko Kita is a departure point for ferry services to Kyushu and the Seto islands. Kayakers working the Nanko canals and the sheltered water behind the breakwaters at Osakako find the tidal current manageable but real — the bay has enough range to move water through its channels at a paddle-relevant pace. The Akashi Kaikyo Bridge crossing, 90 minutes by rail west of Osaka station, spans the Akashi Strait where tidal streams routinely exceed 4 knots on spring tides; the underwater currents are studied by fishers and vessels transiting between the bay and the Hiroshima direction. The Osaka waterfront is primarily an urban and commercial coast. Osaka Bay handles container traffic through the Kobe-Osaka port complex, one of the busiest in Japan. The shoreline from Sakishima south through the artificial islands of the Universal Studios area and west toward Kobe's Port Island is heavily engineered — reclaimed land, breakwater-enclosed harbours, and the former Expo '70 site at Senri, inland but historically part of the bay's industrial hinterland. Shore fishing happens from the breakwaters at Osakako and the rocky points at Kobe and Suma to the west, where black seabream and horse mackerel hold in the tidal currents around structure. The inner Osaka waterfront, from Namba south to the bay via the Namba Parks and the Nanko ferry terminals, is a leisure coast that most visitors to Osaka don't connect to the tides at all. The Dotombori canal, running through the city centre, is a few kilometres inland of the bay and sits at effectively fixed river level, disconnected from direct tidal influence by weirs and sluices. The visible tidal action is on the outer coast: the Sakishima quays at Kaiyukan, the Tempozan harbour, and the ferry berths at Nanko. Weather is the other variable. Osaka Bay is exposed to typhoon approach from the southwest and south; the 1934 Muroto typhoon produced storm surge inside the bay that killed more than 2,000 people, and the current storm-surge flood-wall and gate system protecting the Osaka lowlands — parts of which lie below sea level — reflects that history. The Japan Meteorological Agency issues surge advisories for Osaka Bay, and the forecast matters more than the predicted tide during typhoon season. Predictions on this page come from Open-Meteo Marine, a gridded global ocean model calibrated across a grid cell rather than at the Osaka gauge directly. Accuracy is typically within plus or minus 45 minutes on timing and 0.2 to 0.3 m on height — model-derived, not a local gauge. The Japan Coast Guard and Japan Meteorological Agency maintain the authoritative Osaka tide record; for navigation, commercial ferry scheduling, and storm-surge critical decisions, those official sources apply.