Mughsayl Beach 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 02:00 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/Muscat local. Folk tradition, not a scientific forecast.

Mughsayl Beach lies 35 km west of Salalah, where the Dhofar coast makes a long, open SW-facing arc backed by limestone cliffs 20–40 m high. The beach is one of the finest on the Omani coast: a broad expanse of pale sand that extends for 4 km between rocky headlands, with the Qara Mountain foothills receding inland. The beach is synonymous in Oman with the khareef season, not because it is swimmable during the monsoon — it emphatically is not — but because the blowholes in the limestone platform west of the main beach are the dramatic natural spectacle that draws visitors from across the region. The tidal regime is mixed semidiurnal, spring range approximately 1.5–2.0 m above Chart Datum. The beach faces directly SW into the Arabian Sea; the wide, gently sloping sand floor means the tidal change translates into 80–120 m of horizontal beach movement between the spring high-water mark and the spring low. At low water the exposed sand flat is firm, dry, and walkable for the full distance. The limestone platform to the west of the beach access point carries a series of sinkholes and fissures — the blowholes — where the wave action forces compressed air and water up through the rock. During the khareef (June–September), SW swell arrives from the Southern Ocean fetch across the full Arabian Sea, reaching significant wave heights of 2.5–4.0 m at Mughsayl. The blowholes erupt at 30–90 second intervals, shooting water and spray 10–20 m into the air; the sound carries several hundred metres. The viewing area is a raised car park above the cliff; the limestone platform itself is fenced off during the khareef due to surge risk. Outside the khareef (October–May) Mughsayl is a completely different place: calm, clear water, firm sand, and moderate waves that allow swimming and beach fishing. The blowholes still function on days with swell above 0.8 m but without the monsoon-season spectacle. The beach is at its widest at spring low tide in the October–May dry season; the two-to-three hour window centred on the predicted low gives the best walking conditions on the full beach expanse. Kayaking and snorkelling are possible at Mughsayl in the dry season from the sheltered eastern end of the beach, where the headland provides some swell shadow. The rocky reef at the eastern headland base carries typical Gulf of Oman reef species at depths of 3–8 m. Tidal current at the headland tip can run 0.5–1.0 knots at springs; time snorkelling excursions to avoid the peak ebb when current is strongest. Tide predictions here come from Open-Meteo Marine: accuracy ±45 min / ±0.2–0.3 m. The National Hydrographic Office of Oman publishes official tide tables; Salalah Port is the reference station for this section of coast. The road from Salalah to Al Mughsayl (Highway 47) runs 35 km west along the coast, passing the smaller beach at Ayn Athum and the wadi crossings before arriving at the Mughsayl blowhole car park on the cliff above the beach. The car park is elevated 10–15 m above the beach level and gives a clear view of the blowhole platform and the beach arc. During the khareef, the car park fills with domestic tourists from across Oman and the Gulf; organised food and drink vendors operate from the roadside. Outside the khareef the car park is often empty and the beach access path to the sand is open. The limestone coastal platform at Mughsayl is part of the Khareef Formation, a series of Cretaceous-era limestone units that dominate the Dhofar coast. The blowholes exploit weakness planes in the limestone — natural joints and fractures that the sea has enlarged over millennia of wave action. New vents form occasionally as the sea exploits fresh fracture planes; the platform is geologically active and the blowhole configuration changes on a decadal time scale. The dry-season platform, when wave action is low, gives a clear view of the fissure geometry that explains the blowhole mechanism.