El Cóndor 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 19:00 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/Argentina/Buenos Aires local. Folk tradition, not a scientific forecast.

Next spring tide on Thu 07 May (range 3.5m). Next neap on Fri 08 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.

El Cóndor is a small coastal settlement at the mouth of the Río Negro, 30 km south of Viedma on the North Patagonian Atlantic coast. The Río Negro is the second-largest river in Argentina by volume; its mouth at El Cóndor opens to the South Atlantic through a broad, sandy estuary. The cliffs on both sides of the river mouth — particularly the north cliff — are the site of the largest burrowing parrot (Myiopsitta monachus) colony in the world: an estimated 35,000–50,000 pairs nest in the sandstone bluff, producing a continuous cloud of green-and-grey birds and a constant noise audible several hundred metres away. The tidal regime at El Cóndor is macrotidal semidiurnal; spring range is approximately 3.5–4.5 m above Chart Datum. This is smaller than the San Antonio Oeste range 300 km to the north — El Cóndor is exposed to the open South Atlantic rather than enclosed within the San Matías Gulf, and the Gulf's amplification effect does not extend this far south. Two nearly equal highs and two nearly equal lows occur each day; the range varies predictably through the spring-neap cycle. The Río Negro mouth at El Cóndor is an active estuarine environment: the river's freshwater discharge meets the South Atlantic tidal pulse. The flood tide runs upstream in the Río Negro for 30–40 km from the mouth; estuary salinity and water depth at the crossing point both change markedly through the tidal cycle. The beach on the Atlantic side of the river mouth — Playa El Cóndor — is a broad, exposed south-facing beach that receives South Atlantic swell. At spring low water the beach extends 200–300 m seaward of the high-water mark; at spring high water the beach is minimal. The burrowing parrot colony in the cliffs is accessible from a boardwalk and lookout on the north cliff. The colony is most active in the mornings (07:00–10:00) and late afternoons (17:00–19:00) when the birds return to the cliff from feeding inland. Tide state does not directly affect the parrot colony, but a morning low-tide visit allows the best combination of parrot activity and beach access on the exposed flat below the cliffs. Fishing in the Río Negro estuary targets pejerrey (Odontesthes argentinensis) and corvina (Micropogonias furnieri) in the brackish zone near the mouth. The most productive windows are the first two hours of the incoming tide, when salt water and bait fish push into the estuary. Shore casting from the beach on the Atlantic side targets the same species in marine water. SHN Argentina publishes tide tables for the Río Negro mouth area; Viedma is the nearest official gauge reference. Predictions here: Open-Meteo Marine, ±45 min / ±0.2–0.3 m. The Río Negro mouth is an important ecological transition zone. The freshwater discharge from the river extends a buoyancy plume into the South Atlantic that is visible as a colour change — olive-brown river water meeting the greenish Atlantic — particularly after rain events in the Río Negro basin. Sea fishing in the plume margin, where the river nutrients meeting marine productivity creates a productive mixing zone, is a traditional Patagonian activity. The current at the river mouth can be strong; boat fishing in the channel during the active flood or ebb requires experience with estuarine currents. The Río Negro itself is a significant river; it drains the northern Patagonian Andes and delivers a substantial freshwater discharge to the South Atlantic throughout the year, with peak flow in spring and autumn following snowmelt events. The freshwater plume from the Río Negro mouth extends 20–30 km offshore in the South Atlantic and is detectable in satellite sea-surface salinity measurements. The river mouth habitat — the brackish zone where the freshwater plume meets the tidal intrusion — is the most productive fishing zone; shore fishing from the beach at El Cóndor works this transition boundary on the incoming tide.