Paphos District

Paphos District covers the southwestern corner of Cyprus, from the sandy and rocky coast around Coral Bay and Peyia in the north, through Paphos Harbour with its medieval castle at the harbour mouth, down past Petra tou Romiou — the offshore sea stacks tied to the Aphrodite myth — toward the boundary with Limassol District at Pissouri Bay. The coast faces west and southwest into the open eastern Mediterranean and across the Levantine basin. Long fetch in southwesterly weather, exposed headlands at Cape Drepano and the Aphrodite coast, and small protected coves at Coral Bay and Lara Bay set the geography. The tide signal along the Paphos coast is very small. Mean astronomical range is roughly 10 to 30 cm — microtidal Mediterranean — and spring tides barely push the upper end. Wind and atmospheric pressure dominate water-level variation. Winter southwesterlies and the Levantine pressure systems can push water level along the Paphos seafront, into the harbour, and against the rocky stacks at Petra tou Romiou by tens of centimetres above or below the predicted line, regardless of the astronomical tide. The Akamas Peninsula at the northern end of Paphos District shelters Lara Bay enough to make it a regular sea-turtle nesting site for loggerheads, and the cycle that matters there is the seasonal nesting calendar, not the daily tide. The Cyprus Department of Lands and Surveys and the Cyprus Ports Authority publish the operational tide and water-level data for the island and are the authoritative reference for harbour pilotage at Paphos and for any activity that depends on precise water level. Predictions on this site come from Open-Meteo Marine — a gridded global ocean model with timing accuracy of about plus or minus 45 minutes and height accuracy of roughly 0.2 to 0.3 metres. On a microtidal coast like the Paphos shore, that uncertainty equals or exceeds the predicted astronomical signal.