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Directional Analysis of the Storm Surge from Hurricane Sandy 2012, with Applications to Charleston, New Orleans, and the Philippines

Fig 3

Measured water levels at Kings Point, Long Island.

The water level without tides is calculated by subtracting the predicted tidal cycle from the observed water levels. The resulting "No tides" curve represents the storm surge generated by wind stress alone.

Fig 3

doi: https://doi.org/10.1371/journal.pone.0122113.g003