Jinshan, Shanghai 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 Asia/Shanghai local. Folk tradition, not a scientific forecast.

Next spring tide on Wed 06 May (range 3.6m). Next neap on Sun 10 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.

Jinshan District (金山区) is the only part of Shanghai that faces the sea with a real beach. While central Shanghai's waterfront is all river, embankments, and cargo terminals, Jinshan sits on the southern edge of the municipality facing Hangzhou Bay (杭州湾) — and Hangzhou Bay is one of the most tidally extreme bodies of water in China. The bay is shaped like a funnel, widest at its mouth where it opens to the East China Sea, narrowing sharply as it pushes west toward where the Qiantang River enters at Hangzhou. Tidal energy amplifies as the incoming wave is forced into an ever-tighter space. Mean spring tidal range at Jinshan runs 5.0–7.0 m. That number puts Hangzhou Bay in the same conversation as the Bay of Fundy and the Severn Estuary — places where the tide isn't a minor daily event but a fundamental fact of how the coast operates. Two full tidal cycles per day, each one exposing and recovering 500–800 m of tidal flat measured from the high-water line at Jinshan. At low spring water the bay floor is a wide, flat expanse of grey tidal mudflat. At high water the sea reaches the sea wall and the beach reappears behind it. The rhythm repeats twice a day, every day, regardless of weather or season. The Jinshan City Beach (金山城市沙滩) is an artificial beach, built on reclaimed coastline with imported sand — the only proper urban beach in Shanghai. Opened to the public in 2007, it gave China's largest city its first accessible seaside within city limits. The contrast with the Bund's railing-and-pavement waterfront is stark. On summer weekends the beach draws families from across the city: 24 million residents, one beach. Arrive early or mid-week if you want space on the sand. The water quality in the bay is not pristine — Hangzhou Bay receives runoff from a heavily industrialised coastline — but the beach is managed and monitored, and swimming in the designated zone is the norm rather than the exception during summer. From the beach, looking south, the offshore oil platforms are visible on clear days — active petroleum extraction rigs operating in the bay. The sight of industrial infrastructure framing a family beach tells you something honest about Hangzhou Bay: it is both one of China's most productive marine zones and one of its most used industrial corridors. Sixty kilometres south, the Qiantang tidal bore (钱塘江大潮) runs on the same hydraulic system that produces Jinshan's extreme tidal range. The bore forms because the bay's funnel geometry creates a tidal wave that reaches the river mouth faster than the river can accommodate it — the result is a breaking wave of tidal water that runs upstream, reaching heights of 1–3 m in the best viewing sections near Haining during the autumn equinox. The bore's timing is predictable from the lunar calendar, and the September–October viewing season draws large crowds to the Haining riverbank. Understanding the bore and understanding the range at Jinshan are the same problem: they're both expressions of the bay's geometry concentrating tidal energy. For beach families, the practical question is where in the tidal cycle to plan a visit. At high spring water the beach is full — the imported sand is above water, the swimming zone is open, the food vendors along the promenade are active. At low water the flat extends far beyond the normal waterline and beachcombing is possible, but the exposed sediment is not the beach proper. Check the tide before you drive 40 km from central Shanghai: a low-spring-tide arrival at midday gives you flat mud, not sand. Photographers find the bay compelling at the transition moments — the flood tide returning fast across the flat in the last hour before high water, the offshore platforms silhouetted at dusk, the contrast between the enormous sky and the flat horizon that the funnel-shaped bay opens up. The bay has no strong surf (the flat bottom dissipates wave energy), so photographers can work the waterline without worrying about conditions. Anglers fish the promenade wall and the adjoining rocky structures for yellow croaker and sea bass. The tidal current through the bay runs hard on spring tides — local anglers weight their rigs accordingly and fish the hour of slack around the tide turns. The bay's high turbidity means lure fishing in clear water isn't the technique here; bait fishing on the bottom through the last hour of ebb is the standard approach. Tide data for Jinshan, Shanghai comes from the Open-Meteo Marine API, a gridded model product. Timing accuracy is ±45 minutes, height accuracy ±0.3 m — usable for trip planning, not for navigation.