Sarandë 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 Europe/Tirane local. Folk tradition, not a scientific forecast.

Sarandë is the southernmost significant coastal town in Albania, positioned on a crescent bay on the Ionian shore and separated from Corfu by the Corfu Channel — a stretch of open water that narrows to about 3.5 kilometres at its closest point near the Ksamil beaches. The fast passenger ferry between Sarandë and Corfu town runs the crossing in around 35 minutes, which makes Sarandë the most internationally accessible point on the Albanian coast and the main entry point for visitors coming from Corfu and the broader Greek island chain. The town itself occupies the hillside rising from the harbour and the flat promenade along the bay, and the morning view from the Lekursi castle on the headland above the town looks directly across the Corfu Channel to the Greek island, the proximity making the border more geographic curiosity than barrier. South of Sarandë, the coast runs past the Monastery of Forty Saints on the hill above the shoreline to the Ksamil peninsula and its complex of small beaches, lagoon channels, and offshore islets. The Ksamil coast is the most photographed stretch of the Albanian Riviera: clear shallow water over white sand between limestone headlands, the three uninhabited islets within swimming or kayaking distance from the main beach, and the Butrint Lake lagoon system behind the beach strip, visible from the coastal road. Butrint National Park, 18 kilometres south of Sarandë, is a UNESCO World Heritage Site — a Greek, Roman, Byzantine, and Venetian city built on a wooded promontory between Butrint Lake and the Vivari Channel, with walls, a theatre, a baptistery, and a lion gate spanning twenty-five centuries of continuous occupation. The site is among the most complete ancient coastal settlements in the Mediterranean and receives a substantial share of the visitors who come to Sarandë specifically for the combination of coast and archaeology. The tidal signal at Sarandë is the Ionian open-sea semidiurnal: mean range roughly 0.2 to 0.4 metres, slightly smaller than the Adriatic signal at Vlorë to the north. Two highs and two lows daily, with spring tides pushing toward the upper end of the range and neap tides compressing toward 0.15 to 0.2 metres. On the shallow sandy beaches at Ksamil, the tidal range is enough to shift the tide line visibly — the lowest spring lows expose patches of seagrass and rock that are normally knee-deep, and the wide sandy shelf that extends from the main beach at Ksamil to the islets covers and uncovers perceptibly through the daily cycle. Kayakers doing the Ksamil islet circuit and the Butrint Lake circumnavigation route time the Vivari Channel transit carefully. The Vivari Channel is the narrow tidal connection between the open Ionian Sea and Butrint Lake: 20 to 30 metres wide, deeper in the centre, and the only water exchange point for the entire lake system. The tidal current through the channel on the flood and ebb is perceptible — upstream on the flood, downstream on the ebb — and noticeably stronger than anything on the open coast, where the tidal stream is negligible given the small range. The channel transit is straightforward at slack water around the turn of tide and becomes a meaningful upstream effort on a strong ebb in a loaded sea kayak. Anglers working the Sarandë coast target seabream and mullet from the rocks below the promenade and from the small headlands south of town, timing the session to the last hour of the incoming tide and the first hour of the high. The rocky coast below the Lekursi headland, accessible by foot from the castle or by dinghy from the harbour, holds octopus in the rock crevices and is worked by free divers who operate at low water when the shallow-water zone extends furthest. Corfu visible across the channel means that the sea-state reference many Sarandë-based operators use is the Corfu forecast from the Greek Meteorological Service — the two shores share the same weather system, and the Corfu marine forecast is more detailed and more frequently updated than what is available from the Albanian Meteorological Authority for the Sarandë coast specifically. A northerly in the Corfu Channel compresses between the two shores and can build a steep, short sea on the crossing within 90 minutes of the wind freshening — the ferry service suspends when the channel conditions deteriorate, and the suspension is driven by wave height, not tidal state. The predictions on this page come from Open-Meteo Marine, a gridded global ocean model. Accuracy is typically within plus or minus 45 minutes on timing and 0.2 to 0.3 metres on height — model-derived, not a local gauge. At Sarandë, with a mean range of 0.2 to 0.4 metres, the timing uncertainty is the more operationally relevant figure for activities like the Vivari Channel transit and the Ksamil beach-shelf timing.