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Wind setup information


Effect of wind setup during Hurricane Katrina in 2005

Wind setup, also known as wind effect or storm effect, refers to the rise in water level in seas or lakes caused by winds pushing the water in a specific direction. As the wind moves across the water's surface, it applies a shear stress to the water, prompting the formation of a wind-driven current. When this current encounters a shoreline, the water level along the shore increases, generating a hydrostatic counterforce in equilibrium with the shear force.[1][2]

During a storm, wind setup is a component of the overall storm surge. For instance, in the Netherlands, the wind setup during a storm surge can elevate water levels by approximately 3 metres above the normal tide. In the case of cyclones, the wind setup can reach up to 5 metres. This can result in a significant rise in water levels, particularly when the water is forced into a shallow, funnel-shaped area.[3]

  1. ^ Smith, S.D. (1988). "Coefficients for sea surface wind stress, heat flux, and wind profiles as a function of wind speed and temperature". Journal of Geophysical Research: Oceans. 93 (C12): 15467–15472. Bibcode:1988JGR....9315467S. doi:10.1029/JC093iC12p15467. Retrieved 26 June 2023.
  2. ^ Garvine, R.W. (1985). "A simple model of estuarine subtidal fluctuations forced by local and remote wind stress". Journal of Geophysical Research: Oceans. 90 (C6): 11945–11948. Bibcode:1985JGR....9011945G. doi:10.1029/JC090iC06p11945. Retrieved 26 June 2023.
  3. ^ Verboom, G.K.; van Dijk, R.P.; deRonde, J.G. (1 November 1987). "Een model van het Europese Kontinentale Plat voor windopzet en waterkwaliteitsberekeningen" [A model of the European Continental Shelf for wind setup and water quality calculations]. Z0096 (in Dutch). Deltares (WL). Retrieved 26 June 2023.

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