Three-dimensionality of shallow island wakes

  • Paul M. BransonEmail author
  • Marco Ghisalberti
  • Gregory N. Ivey
Original Article


Island wakes are thought to play a significant role in the vertical and cross-shelf mixing processes in strong tidally forced coastal regions. This paper describes a comprehensive laboratory study of shallow water wakes behind islands of circular cross section forced by a sinusoidal tidal flow. The wake structure and vertical circulation are determined through novel three-dimensional particle imaging velocimetry measurements. Four archetypal wake forms (symmetric, asymmetric, unsteady bubble, and vortex shedding) are observed. Through examination of the vertical structure of each of these wake forms, we demonstrate the dependence of vertical transport in island wakes on three key parameters: (1) the tidal excursion relative to the island size, (2) the bottom boundary layer thickness relative to the flow depth and (3) the aspect ratio of the island size to the flow depth. The importance of secondary vortices in island upwelling is highlighted by local peaks in vertical velocity that exceed 40% of the peak external tidal velocity. This study fundamentally changes the view of island wake upwelling from a weak ‘tea cup’-like recirculation process to one where primary and secondary flow structures vigorously stir the water column over the full depth. This has fundamental implications for the fate of passive biological tracers and the time scales that determine productivity in topographically-complex continental shelf regions.


Island wakes Three dimensional flow Tidal forcing Upwelling Vorticity 



P. M. Branson gratefully acknowledges the support of a University Club of Western Australia Research Travel Scholarship to attend the 4th International Symposium on Shallow Flows. The authors acknowledge numerous insightful discussions with E. J. Hopfinger during his visit to UWA on a Gledden Visiting Fellowship. This work was supported by resources provided by the Pawsey Supercomputing Centre with funding from the Australian Government and the Government of Western Australia. We acknowledge the use of imagery provided by services from the Global Imagery Browse Services (GIBS), operated by the NASA/Goddard Space Flight Center Earth Science Data and Information System (ESDIS) project. Funding was provided by Australian Research Council Discovery Project (Grant No. DP1095294).


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Copyright information

© Springer Nature B.V. 2019

Authors and Affiliations

  1. 1.Oceans Graduate SchoolUniversity of Western AustraliaCrawleyAustralia

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