Stavanger 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.

Marine-conditions data not available for this station. Wind, swell and water temperature ride along with Open-Meteo Marine; gauge-only stations (e.g. UK EA Flood) publish water level only.

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 Europe/Oslo local. Folk tradition, not a scientific forecast.

Stavanger occupies a peninsula at the edge of the Boknafjord, surrounded by an archipelago so fragmented it is easier to count the passages between islands than the islands themselves. The city's double identity — old wooden town of painted merchants' houses on one side, global oil capital on the other — has shaped the waterfront in ways visible from any boat passing the harbour mouth. Offshore supply vessels, crew-transfer boats, and the occasional seismic survey ship share the approaches with recreational fishing boats and the archipelago ferries that thread between the islands toward Tau and Jelsa. Lysefjord, the fjord that draws the tourists, starts about 25 kilometres from Stavanger by water, cutting east through increasingly steep walls until the cliffs at Preikestolen rise straight from the surface. The tide in Stavanger is semidiurnal — two highs and two lows per day — with a mean spring range of approximately 0.6 to 0.8 metres. That modest range is unremarkable in isolation, but Rogaland's geography means it matters in context. In open water across the Boknafjord, the 0.7-metre spring tide produces tidal streams of 0.3 to 0.5 knots — calm water, generally. In the narrows between islands, where the same volume of water moves through a gap a fraction of the width, streams run 1.5 to 3 knots on springs. The Mastrafjord, the passage east of Stavanger toward the fjord system, concentrates tidal flow noticeably. Kayakers crossing between islands plan crossings with the stream rather than across it. Small fishing boats run timed departures through the island gaps at slack or with the flood, depending on direction. In Lysefjord itself, the tidal influence is present but quiet through most of the fjord's 42-kilometre length. The walls are close enough in several places that shade falls across the water for hours mid-day in winter, and the waterfalls — Hengjanefossen and several unnamed seasonal falls — drop freshwater directly into the fjord year-round. That freshwater stays on the surface, less dense than the salt water below, creating a halocline at depth that divers encounter as a blurred visibility layer. Boat tour operators running from Stavanger out to Preikestolen base departures on weather windows more than tidal state, but passage through the outer skerry narrows does get timed around stream conditions. Fishing in Rogaland covers the full range: jigging for saithe and cod in the island channels from mid-summer through autumn, mackerel shoals in the outer Boknafjord from June onward, and pollock working the current lines behind the skerry edges. The fish follow the tidal current at the pinch points. Shore fishing from island rocks at the mouth of active narrows — the locals call it merking, marking a spot — works best on the ebb when current acceleration concentrates prey. Kayak fishing has grown significantly over the past decade, and the inner archipelago with its numerous protected coves and accessible passages is well-suited to it. The water temperature runs 12 to 17 degrees Celsius through summer, cold enough that a wetsuit is appropriate for extended immersion even on a warm August afternoon. Swimmers use the sheltered coves within the archipelago rather than open water — Solastranden south of Stavanger airport is the main swimming beach, a kilometre of sand facing southwest, open to any south or southwest swell but sheltered from northwest by the peninsula. The tidal change is 0.6 metres spring range, which shifts the beach width meaningfully at a flat beach: 50 metres of dry sand at high water becomes 80 metres at low, with a sandbar exposed in the gentler conditions. Photographers working the coastline come for the evening light on the granite skerries near Sola and Tananger, and for the winter conditions when the Boknafjord surface goes flat in calm freezing air and the light quality around the winter solstice is unlike anything on a lower-latitude coast. The Norwegian Meteorological Institute's Yr.no service provides combined tide and weather forecasts for this coast, and the Norwegian Mapping Authority (Kartverket) publishes the authoritative tidal current tables for the island narrows and fjord passages. Tide predictions on this page come from Open-Meteo Marine, a global gridded ocean model — typically accurate within plus or minus 45 minutes on timing and 0.2 to 0.3 metres on height, model-derived, not a local gauge. For the outer Boknafjord and Stavanger harbour area, that accuracy is generally sufficient for recreational planning. For the inner narrows and fjord passages where tidal current timing matters, Kartverket's local tables are the authoritative reference.