Alanya, Antalya 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/Istanbul local. Folk tradition, not a scientific forecast.

Alanya's 250 m promontory is one of the most visually dominant features on the Turkish Mediterranean coast. The headland rises abruptly from the sea, steep on all sides, with the Seljuk castle (Alanya Kalesi) running along its ridge and dropping in curtain walls to the water. From the castle walls on a clear morning you can see 30 km of coast in both directions — the flat Cilician plain to the east, the beginning of the Taurus foothills to the west. The promontory divides everything, including the beaches. Cleopatra Beach runs for about 3 km to the west of the promontory, sheltered from the northeast by the headland mass. It faces southwest, catches the afternoon sun, and has the fine sand and calm-water character that makes it the default choice for families and resort guests. The eastern beach — officially Keykubat Beach — faces northeast and gets the full fetch of the Poyraz (northeast) swell in winter. In summer both beaches are calm; in November through February, Keykubat can have 1-2 m shore-break while Cleopatra sits flat. The tidal regime here is Eastern Mediterranean microtidal. Mean range is 0.2-0.3 m, mixed semidiurnal — two high and two low waters per day of unequal height. Spring tides (around new and full moon) push the range to perhaps 0.35 m, neap tides drop it to 0.15 m. In practical terms, this is a barely perceptible tide. The beach width at Alanya does not visibly change between high and low water; the tide is not the variable that determines whether a rock shelf is accessible or a sandbar is above water. What does move is atmospheric-driven water level: a deep low-pressure system in the eastern Mediterranean can raise the Alanya waterline by 20-30 cm above predicted. Combined with a 0.3 m spring tide, that produces a total water level approaching 0.6 m above mean — still modest by Atlantic standards, but noticeable if you are working off rock ledges. Damlataş Cave is cut into the promontory at sea level on the southwest side, between the harbour and the base of the headland. The cave is accessible through a tourist entrance that has been open since 1948. The interior humidity is consistently 98% and the CO2 concentration is elevated — the cave was historically promoted as a treatment site for asthma (the claim is contested, but it draws visitors). What is geologically certain is that the cave connects to the promontory's internal water table, which itself sits a few centimetres above mean sea level. During spring tide periods, when the Alanya waterline is at its maximum of approximately 0.35 m above chart datum, the cave's interior humidity measurably increases as the water table responds. It is a subtle but real tidal signature in a coast that otherwise shows almost none. The Red Tower (Kızıl Kule) at the foot of the promontory on the harbour side is the other water-level landmark. Built in 1226 CE under the Seljuk sultan Alaeddin Keykubad, the tower's ground floor was constructed at what was then mean high water — the stone ramp connecting it to the harbour infrastructure was designed to be accessible on foot at most states of the tide (which was already negligible). Today the tower sits approximately 0.5 m above current mean sea level, the difference reflecting a combination of sea-level change and local land movement since the 13th century. The stone ramp is now permanently dry. For anglers, the promontory creates distinct fishing ground. The eastern side of the headland has depth quickly — 20-30 m within 200 m of the cliff base — and holds grouper (lahoz), dentex, and sea bream around the rock structure. The western (harbour) side is shallower and more disturbed by boat traffic. The Damlataş cave mouth opens into an underwater feature that local divers know as a good mark for bream in the 5-10 m zone. Kayakers and paddlers operating from the town beach can explore the sea caves cut into the base of the promontory — Pirates Cave (Korsanlar Mağarası), Phosphorus Cave (Fosforlu Mağara), and Lovers Cave (Aşıklar Mağarası) are all accessible by sea from the harbour. Commercial boat tours run hourly. Because the tidal range is 0.2-0.3 m, the cave access heights are essentially constant — the cave entrances do not become impassable at any predictable tidal state. The variable is wave height: 0.5 m swell makes the cave entrances comfortable, 1.5 m (Poyraz conditions) closes them. Photographers working the castle at golden hour have a reliable geometry: the 250 m promontory catches the last light long after the town beach has gone into shadow, and the Red Tower's ochre masonry reads well against the blue harbour water. The fixed water level means the harbour foreground is the same at 17:00 as at 19:00. Tide data for Alanya, Antalya 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.