Karlskrona 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 01:00 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 Europe/Stockholm local. Folk tradition, not a scientific forecast.

Karlskrona is built on a cluster of islands and peninsulas at the southern edge of Sweden's Blekinge coast, where the Baltic Sea opens south. The city was founded in 1680 by King Charles XI as a naval base; its regular grid streets, baroque naval buildings, and the Amiralitetskyrkan wooden naval church all date from this founding era. The entire naval town was inscribed as a UNESCO World Heritage Site in 1998. Marinbasen Karlskrona is Sweden's second-largest active naval base. The tidal regime at Karlskrona is essentially non-tidal. The Baltic Sea's narrow connection to the North Sea through the Danish straits allows negligible tidal exchange; mean tidal range at Karlskrona is approximately 10 cm. Water level change is governed almost entirely by wind-driven setup and atmospheric pressure: a sustained southwesterly gale can raise Karlskrona's water level by 0.4–0.6 m above mean; a strong northeasterly can lower it by a similar amount. The Open-Meteo tide predictions for Karlskrona represent a combination of the negligible astronomical tide and the dominant meteorological water level signal. For boaters, the near-zero tidal range means anchoring depth calculations are essentially static — the water level on arrival is the water level overnight, within ±0.1 m barring weather change. Mooring lines at the Karlskrona guest harbour need no tidal scope adjustment. What does require attention is wind-driven surge: an overnight southwesterly developing to gale force can raise the harbour water level by 0.3–0.4 m, relevant for boats moored close under fixed walkways or bridges. The archipelago south of Karlskrona — the Karlskrona skärgård — stretches 20–30 km into the southern Baltic and contains hundreds of small granite islands. This archipelago is the primary recreational asset of the coast, used extensively by sea kayakers, day sailors, and motorboat operators from May through September. The non-tidal nature of the water means there is no current planning involved — you read the wind and the chart, not the tide table. Fishing in the Karlskrona area targets Baltic cod and flatfish (flounder, dab) on the sandy bottom between the outer islands, and perch and pike-perch in the inner brackish channels. Baltic cod populations have declined significantly; seasonal quotas and minimum size limits are strict. Perch fishing from the inner island channels is productive in June and September, when the shallow brackish water warms and fish feed aggressively. Tidal state does not affect the fishing; wind direction and temperature are the relevant variables. Ferries from Karlskrona run to Gdynia in Poland (Stena Line overnight service, approximately 10 hours) — one of the main truck and passenger ferry routes across the southern Baltic. These ferry operations are unaffected by tidal conditions. All tide predictions for Karlskrona come from the Open-Meteo Marine gridded model. Timing accuracy is ±45 minutes; height accuracy is ±0.3 m above Chart Datum.