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Playa Santa Teresa ratings
Quality on a good day: 3.8
Consistency of Surf: 4.2
Difficulty Level: 2.6
Wind and Kite Surfing: 2.0
Crowds: 2.8

See all 18 ratings

Based on 5 votes. Vote


Surf Report Feed

The rose diagram shows how often and how strongly the wind blows from different directions through a typical July. The longest spokes point in the directions the wind most commonly blows from and the shade of blue indicates the strength, with dark blue strongest. It is based on 1736 NWW3 forecasts of wind since since 2006, at 3hr intervals, for the closest NWW3 model node to Playa Santa Teresa, located 23 km away (14 miles). There are insufficient recording stations world wide to use actual wind data. No doubt some coastal places have very localized wind effects that would not be predicted by NWW3.

According to the model, the most common wind at Playa Santa Teresa blows from the WSW. If the rose plot shows a nearly round shape, it means there is no strong bias in wind direction at Playa Santa Teresa. Converseley, dominant spokes show favoured directions, and the more deep blue, the stronger the wind. Spokes point in the direction the wind blows from. Over an average July, the model suggests that winds are light enough for the sea to be glassy (pale blue) about 0.3% of the time (0 days each July) and blows offshore just 0.3% of the time (0 days in an average July). During a typical July winds exceeding >40kph (25mph) are not expected, but 0 have winds on the range 30-40 (19-25) at Playa Santa Teresa

IMPORTANT: Beta version feature! Swell heights are open water values from NWW3. There is no attempt to model near-shore effects. Coastal wave heights will generally be less, especially if the break does not have unobstructed exposure to the open ocean.

The Pacific Tsunami Warning Center has stated that a magnitude 8.2 Earthquake beneath the Sea of Okhosk did not generate a destructive Tsunami. However, we suggest that local interests also listen for statements from the Japan Meteorological Agency, located much closer to the source.

 

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