Limassol District

Limassol District covers the central southern coast of Cyprus, from the wide sweep of Akrotiri Bay and the Akrotiri Peninsula at the western end through the Limassol seafront and Old Port to the village beaches at Pissouri and the headlands toward Paphos District. The coast faces south into the open eastern Mediterranean — the basin of water between Cyprus, the Levantine coast, and the African shore — and that geography sets the conditions for everything: long fetch in southerly weather, calm summer mornings, and a tide signal that is essentially negligible. Cyprus is a microtidal coast in the strictest sense. Mean astronomical tide range along the Limassol seafront is in the order of 10 to 30 cm, and spring tides only push that toward the upper end of the band. Wind and atmospheric pressure dominate water-level variation absolutely. A sustained southerly during winter or a deep low pressure crossing the eastern Mediterranean can push water levels along Akrotiri Bay and into the Old Port 30 to 50 cm above the predicted level — more than the entire predicted tide range, in any direction. The Akrotiri Salt Lake complex behind the peninsula, fed by seasonal rainfall and connected to the sea by the narrow Akrotiri channel, exhibits its own water-level cycle driven primarily by evaporation and rainfall rather than by the marine tide. The Cyprus Department of Lands and Surveys, together with the Cyprus Ports Authority, publishes the operational tide and water-level data for the island's coast and is the source of record for harbour pilotage, marina operations, and coastal-event scheduling. 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. For a coast with this small a tidal signal, the model uncertainty is a meaningful fraction of, and often larger than, the actual astronomical movement.