Wind setup

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, lakes, or other large bodies of water caused by winds pushing the water in a specific direction. As the wind moves across the water’s surface, it applies shear stress to the water, generating a wind-driven current. When this current encounters a shoreline, the water level increases due to the accumulation of water, which creates a hydrostatic counterforce that balances the shear force applied by the wind.[1][2]

During storms, wind setup forms part of the overall storm surge. For example, in the Netherlands, wind setup during a storm surge can raise water levels by as much as 3 metres above normal tidal levels. In tropical regions, such as the Caribbean, wind setup during cyclones can elevate water levels by up to 5 metres. This phenomenon becomes especially significant when water is funnelled into shallow or narrow areas, leading to higher storm surges.[3]

Examples of the effects of wind setup include Hurricanes Gamma and Delta in 2020, during which wind setup was a major factor when strong winds and atmospheric pressure drops caused higher-than-expected coastal flooding across the Yucatán Peninsula in Mexico.[4] Similarly, in California’s Suisun Marsh, wind setup has been show to be a significant factor affecting local water levels, with strong winds pushing water into levees, contributing to frequent breaches and flooding.[5]

  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.
  4. ^ Torres-Freyermuth, A.; Medellí, G.; Kurczyn, J.A.; Pacheco-Castro, R.; Arriaga, J.; Appendini, C.M.; Allende-Arandía, M.E.; Gómez, J.A.; Franklin, G.L.; Zavala-Hidalgo, J. (2022). "Hazard assessment and hydrodynamic, morphodynamic, and hydrological response to Hurricane Gamma and Hurricane Delta on the northern Yucatán Peninsula". Natural Hazards and Earth System Sciences. 22 (12): 4063–4085. Bibcode:2022NHESS..22.4063T. doi:10.5194/nhess-22-4063-2022.
  5. ^ Algra, S.; Huijbregts, J.; Prins, S.; Terliden-Ruhl, L.; Lanzafame, R.C.; Pearson, S.G. (2023). Risk Analysis: Van Sickle Island (Multidisciplinary Project Report: Group MDP 350). Delft University of Technology. Retrieved 27 September 2024.