Punta del Este 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 America/Montevideo local. Folk tradition, not a scientific forecast.

Last spring tide on Fri 15 May (range 0.6m). Next spring tide on Thu 21 May (range 0.9m). Next neap on Mon 18 May.

Spring tides cluster around new and full moons (biggest swings). Neap tides land on quarter moons (smallest swings). See the spring tide and neap tide glossary entries for the why.

Punta del Este is a narrow finger of land — the peninsula is barely 500 m wide at its narrowest — extending south from the Uruguayan coast to divide the open Atlantic from the inner Río de la Plata estuary. The finger-tip position gives the town two entirely different coastal personalities: Playa Brava on the Atlantic side faces east-northeast, collecting the South Atlantic groundswell; Playa Mansa on the estuary side faces west-northwest into the calmer, more sheltered Plata water. The same tide prediction applies to both sides, but wave height, current, and water clarity differ enough that the two beaches feel like separate places. The tidal regime at Punta del Este is meso-tidal semidiurnal. Spring range is approximately 1.0–1.4 m above Chart Datum; neap range 0.5–0.7 m. This is genuinely oceanic tide — the peninsula is far enough from the Plata estuary mouth that the astronomical signal is relatively clean, uncontaminated by the surge-dominated regime that affects Montevideo 100 km to the west. The range is still modest, and the beach width changes visibly with the tide: Playa Brava exposes an additional 20–30 m of sand at low water; Playa Mansa, being shallower and more gently sloping, exposes 30–50 m. Playa Brava is the surf beach. The break is a beach break that responds to South Atlantic groundswell from the SE and E; the best conditions are on the incoming tide when wave shape is cleanest. Rip currents form between the sand banks at mid-tide; the beach has seasonal lifeguard coverage from December through February (the Uruguayan summer). Playa Mansa is the calmer, family beach; the water is warmer (the Plata water retains summer heat better than the open Atlantic) and the surface is usually flat. The Isla Gorriti, 1 km offshore in the Mansa bay, is accessible by water taxi from the Mansa marina. The crossing takes 10 minutes; the island has two small beaches facing opposing directions, giving sheltered water on one side regardless of wind direction. At spring low tide a sand bank partially emerges between the island and the peninsula tip, reducing the crossing depth to around 1.5 m — still navigable by the water taxis, but notable for kayakers who make the crossing independently. The port of Punta del Este, at the peninsula tip, handles yacht traffic from around the South Atlantic; the famous biennial ocean race Velux 5 Oceans and the Jules Verne record attempts use Punta del Este as a waypoint. The inner yacht basin is sheltered from both sides; tidal range inside the harbour is the same as the open coast. Fishing off the Rambla and rocky points at the peninsula tip targets corvina (Micropogonias furnieri), pejerrey (Odontesthes argentinensis), and occasionally the larger lenguado (flounder) on the incoming tide. The best shore-casting windows are from one hour before to two hours after the predicted low, fishing the rising water. SOHMA (Servicio de Oceanografía, Hidrografía y Meteorología de la Armada) publishes official Uruguayan tide tables. Predictions here come from Open-Meteo Marine: accuracy ±45 min / ±0.2–0.3 m. The famous La Mano sculpture (La Mano Emergiendo de la Arena, by Mario Irarrázabal, 1982) is buried in the Playa Brava sand with five concrete fingers pointing skyward — photographed by every visitor, and noticeably more or less buried depending on the sand accretion cycle. The sculpture sits above the high-water line; at spring high tide with elevated surge, wave wash reaches the base of the sculpture fingers. The relationship between tide, storm surge, and how much of the 'hand' is visible above the sand is a micro-version of the same coastal dynamics that govern the whole beach.