Hiroshima 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.

Last spring tide on Sat 02 May (range 2.5m). 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.

Hiroshima lies at the head of Hiroshima Bay on the northern coast of the Seto Inland Sea, where the Ota River delta fans out across a flat coastal plain and a scatter of small islands extends south toward Miyajima and the broader sea beyond. The Seto Inland Sea — Setonaikai — is one of the world's most geographically complex tidal environments: a 450 km enclosed sea connecting to the Pacific through the Kii and Naruto Channels in the east and through the Kanmon Strait near Kitakyushu in the west, with more than 3,000 islands creating a labyrinth of channels, shallows, and constrictions. The tidal character it produces is semidiurnal — two roughly equal highs and two roughly equal lows per day — with a mean range in Hiroshima Bay of approximately 1.5 to 2.0 m. That range, combined with the gently-shelving seabed of the inner bay and the many island-enclosed tidal flats, means the sea-level change is visible in a way it is not on microtidal coasts. And nowhere in the Seto Inland Sea is the tide's visual consequence more famous than at Miyajima Island, 20 km southwest of Hiroshima city by ferry. Miyajima — officially Itsukushima — holds the Itsukushima Shrine, a Shinto complex built over the water that has been a sacred site since the sixth century and a UNESCO World Heritage Site since 1996. The shrine's defining feature is the O-torii, a 16-metre vermilion gate of two great pillars joined by a curved crossbeam, standing in the tidal flat approximately 200 m offshore from the shrine's waterfront walkways. At high tide, water surrounds the gate's base and rises to obscure the lowest structural members: the gate appears to float on the sea surface, the reflection shimmering across calm water. It is one of the most reproduced images in Japan, appearing on postcards, currency, and travel photography across a century of documentation. At low tide, the tidal flat is exposed for 200 to 300 m in front of the gate. The sandy and gravelly bottom, lightly colonised by shore-crabs and small wading birds at the margins, allows visitors to walk out from the shoreline and stand directly at the gate's base, touching the barnacled lower pillars, looking up at the crossbeam 16 m overhead. These are two fundamentally different experiences of the same structure, separated by roughly six hours of tidal cycle. The gate appears to float at high water; it stands on exposed ground at low. The tide makes a landmark change character completely twice each day. Local photography guides consistently recommend arrival two hours before high tide to capture the gate with water around it but still at an angle that catches the crossbeam reflection clearly; at the precise high water, if conditions are calm, the reflection is at its fullest. Two hours after low water, the flat is walkable but not yet fully dried, giving firm sand for a close approach. The tidal height predictions on this page — model-derived from Open-Meteo Marine, typically within plus or minus 45 minutes on timing and 0.2 to 0.3 m on height — are sufficient for planning the visit to within a reasonable window. For the exact minutes of high and low at Miyajima specifically, the Japan Meteorological Agency publishes harmonic predictions for Miyajima station directly. Beyond Miyajima, the Hiroshima waterfront and the Seto Inland Sea ferry network define this coast's practical character. Ferries from Hiroshima's Ujina port serve Matsuyama on Shikoku, the Etajima island, and the island cluster around Osaki Kamijima. Fishing vessels work the tidal channels between islands for sea bream (tai), which is culturally associated with the Seto Inland Sea to the point of being the region's defining seafood. The tidal currents around the island narrows concentrate bream and smaller reef species; sea anglers on the overnight charter boats time their jigging to the tide change windows. Kayaking in Hiroshima Bay and among the inner Seto islands is a growing activity. The island-hopping routes between Hiroshima, Etajima, and the Kure coast to the southeast are covered by paddlers on calm-season trips. The 1.5 to 2.0 m range creates tidal streams through the narrower island passages that require planning: the Nomi Strait between Etajima and the Kure shore runs at 2 to 3 knots on spring ebbs. Experienced paddlers transit narrows at slack water; beginners stay in the sheltered coves and avoid the main channel passages on spring tides. The Japan Coast Guard and Japan Meteorological Agency maintain the authoritative Hiroshima and Miyajima tide records. Predictions on this page come from Open-Meteo Marine gridded ocean modelling — sufficient for activity planning, not a replacement for official data in navigational or safety-critical decisions.