Makarska, Dalmatia 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 00:00 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/Zagreb local. Folk tradition, not a scientific forecast.

Makarska is a resort town in central Dalmatia that owes its character to a single geographic fact: the Biokovo massif rises from sea level to 1762 m within 5 km of the shore. The vertical gradient here is among the steepest in Europe — standing on the main beach you look directly up to rocky ridgelines that catch cloud and snow in winter while the beach below stays dry and 15°C warmer. The Sv. Petar peninsula encloses the bay from the west, and the town's marina and main beach sit in the calm water between the peninsula and the shore. The Adriatic tidal regime at Makarska, like the rest of the mid-Dalmatian coast, is semidiurnal with a mean range of 0.25–0.45 m. The amphidromic system that keeps the central and southern Adriatic microtidal places Makarska in the transitional zone between the near-zero southern node and the higher ranges of the northern basin. In practical terms, the tide here produces predictable, twice-daily cycles with a total height change that is visible but modest. Spring tides reach approximately 0.5 m; neap tides drop to 0.2 m or less. The main town beach — Gradska Plaža — is pebble, as are all the central Makarska beaches. Pebble foreshores on Adriatic beaches respond to the tidal cycle in a way that sand beaches do not: the pebble berm extends and retracts cleanly as the water advances and retreats, and the underwater pebble slope is visible through clear water to depths of several metres. At low water, Gradska Plaža extends 15–20 m further seaward than at high water. The transition is gradual over two to three hours of falling tide, and the pale limestone pebble bottom through 1–2 m of clear water makes the tidal movement easy to track visually — the waterline advances against individual stones in real time. This is one of the few Adriatic locations where a family can concretely watch and explain tidal movement to children without needing instruments. The Sv. Petar peninsula defines the western edge of Makarska bay. The peninsula is a limestone headland roughly 800 m long, connected to the town by a narrow isthmus that carries the coast road. The outer (southwest) face of Sv. Petar is exposed to the open Adriatic and drops vertically into deep water. The dive site along the western face is accessible from the shore on the sheltered north side — a 50 m swim from the rocky entry point at the base of the peninsula, then along the cliff base to the point, where the rock face drops to 25 m in open water. The dive is entry-level in terms of depth but requires comfort with current: the Adriatic tidal current along the Sv. Petar point runs at 0.2–0.4 knots at peak flow, ebbing northwest and flooding southeast. Divers plan entry at slack water, approximately 30–45 minutes after the predicted high or low. The wall supports gorgonian fans from 12 m down, and the horizontal visibility frequently exceeds 20 m. Biokovo Nature Park begins at the edge of town and extends to the summit ridge at Sv. Jure (1762 m). The Makarska coastal path — Šetalište Franjo Tuđman — runs the length of the bay, but the direct ascent trails to Biokovo begin within 2 km of the beach. The Vošac trail from the town ascends approximately 1100 m over 5 km; starting from the coast in the morning and reaching the ridge before the afternoon convective cloud builds is a standard approach. The elevation change between beach and summit is the relevant operating fact for anyone doing sea and mountain in the same day. The Makarska Riviera extends for roughly 60 km between Brela to the north and Gradac to the south. Brela, 15 km north of Makarska, has a more developed beach infrastructure and the iconic Kamen Brela rock — a solitary limestone pillar rising from shallow water just offshore, accessible by a short swim or paddle. The beaches along the Riviera are broadly consistent in character: pebble foreshore with clear water over limestone bottom, consistent tidal range, and the Biokovo wall as the constant backdrop. For anglers, the rock points at either end of Sv. Petar peninsula are the most productive shore stations. The current that runs along the outer face concentrates baitfish; sea bass, dentex, and amberjack hold in the eddies behind the point, particularly in the two hours before and after high water. Spinning gear with surface lures is effective at dusk when the light is low. Night fishing is permitted from the rocks; the headtorch and lure combination typical of Mediterranean shore fishing is the standard approach on the Sv. Petar outer face. Tide data for Makarska, Dalmatia 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.