Coral Bay, Paphos District 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 Asia/Nicosia local. Folk tradition, not a scientific forecast.

Coral Bay is a sheltered arc of sand 8 km north of Paphos town, framed by two low limestone headlands that compress the bay into a shape that holds calm water on most summer days. The beach itself is coarse sand, a pale buff colour that reflects the Cretaceous limestone of the headland cliffs behind it. The name is not metaphorical: the limestone in the headland outcrops contains fossilised coral from the ancient Tethys Sea, visible in cross-section in the roadside cuts along the approach road — discrete coral heads, branching forms, and tabular growths replaced in silica and calcite over tens of millions of years. What remains is the mould, not the original material, but the structures are clear enough that you can identify colony types without any formal training. The tidal regime at Coral Bay is Eastern Mediterranean — mean range 0.1 to 0.3 m, driven primarily by the M2 tidal constituent modulated by meteorological forcing. In practice, the astronomical tide is often the smaller signal: a sustained westerly fetch across the Mediterranean or a drop in pressure of 10 hPa can displace the water surface by more than the full spring tidal range. That said, the systematic tide is present and it matters for what is happening at the bay edges. The submerged rock reefs at the northern and southern headland flanks — extensions of the coral limestone into the sea — show tide-correlated exposure at their shallow inner sections. At average low water, the reef surface in 0.3 to 0.5 m depth becomes visibly clearer to walk over and the seagrass stems at the reef edge stand in less water, making their extent more readable from above. Those reefs are the most ecologically significant feature of Coral Bay from a snorkeller's or diver's perspective. Between the reef edges and the sandy beach, Posidonia oceanica seagrass meadows cover the sandy substrate in a band that runs roughly parallel to the shoreline. Posidonia is a true flowering plant — not an alga — that produces rhizomes building up over centuries into mats called matte, which accumulate to depths of several metres and act as natural breakwaters, slowing current and trapping sediment. The leaves are long, ribbon-like, and produce the rolled balls of dead fibre called aegagropilae that wash up on beaches across the Mediterranean. At Coral Bay the meadows are in good condition in the areas away from anchoring activity; anchor damage is visible in the sandy blow-out patches within the meadow, where rhizomes have been broken and recovery is slow — Posidonia grows at approximately 1 to 6 cm per year. Snorkelling over the meadow from the reef edge toward the beach gives a reliable fish census: two-banded sea bream forage along the meadow-sand boundary, salema move in loose aggregations through the leaf canopy, small grouper use the meadow-reef interface. The water clarity over the sandy bottom in the bay interior is 10 to 15 m on calm days. Entry is easy from the main beach; the reef flanks are best accessed from the water rather than climbing over the headland rocks. The bay is exposed to westerly and southwesterly swell. Cape Drepanum, the limestone promontory at the northern end of the bay, provides some shelter from northwest quadrant swell, but south-to-southwest fetch remains open. Winter storm events — typically December through February — generate swell periods of 6 to 10 seconds and face heights of 1 to 2 m at the beach, which suspends the sediment and drops water clarity to under 5 m for 24 to 48 hours after an event. Summer conditions are stable; afternoon sea breezes from the west build by 14:00 and generate short-period chop across the bay, which subsides by early evening. Small boat hire and pedalo rental operate from the beach during the main season, late April through October. The pedalo zone is marked with buoys and is separate from the snorkelling area at the reef flanks. Boat traffic through the bay increases significantly in July and August; anchor selection outside the marked zones carries a real risk of Posidonia damage, which is prohibited under EU Habitats Directive transposition into Cypriot law. For kayakers, the northern headland route to Cape Drepanum is 2 km from the Coral Bay beach. The headland base has sea caves and arched sections in the limestone at low water accessible by sea kayak — the cave ceilings are low, requiring entry at low tide when 0.3 to 0.5 m of additional clearance is available. The paddle is best timed for the morning before the westerly sea breeze builds. For anglers, the reef edge at the northern headland is the productive ground. From the rocks at the headland base at low water, a cast of 15 to 20 m clears the reef and drops bait onto the sandy edge of the Posidonia meadow, where bream feed. A running ledger with sandworm or prawn is effective; light spinning over the reef top takes wrasse and small grouper. Tide data for Coral Bay, Paphos District 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.