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Large scale circulations in shallow lakes

  • Giuseppe Curto
  • , János Józsa
  • , Enrico Napoli
  • , Giordano Lipari
  • , Támas Krámer

Research output: Chapter in Book/Report/Conference proceedingChapterAcademicpeer-review

Abstract

In this paper wind-driven horizontal and vertical large scale circulations in shallow lakes are analysed

As an improved approximation of the external forcing field, the wind speed acceleration due to the abrupt reduction in the surface roughness between the land and the water is quantified along the fetch using a semi-empirical approach which allows the identification of the aerodynamic features and hydrodynamic effects of an Internal Boundary Layer (IBL) growing within the bottom of the atmospheric boundary layer

The consequent fetch-dependence of the wind speed and corresponding wind shear stresses on the lake surface causes the appearance of a wind stress curl, which is responsible, together with changes in bathymetry, for causing strong horizontal circulations. The effects of wind speed changes on the wind-driven flow patterns are analysed both analytically and numerically, showing the need to take these changes into account in order to correctly predict wind-induced water currents in shallow basins
Original languageEnglish
Title of host publicationVorticity and Turbulence Effects in Fluid Structure Interaction
Subtitle of host publicationAn Application to Hydraulic Structure Design
EditorsM. Brocchini, F. Trivellato
Place of PublicationSouthampton, UK
PublisherWessex Institute of Technology Press
Pages83-104
Number of pages22
Volume45
ISBN (Electronic)978-1-84564-229-7
ISBN (Print)978-1-84564-052-1
Publication statusPublished - 2006
Externally publishedYes

Publication series

NameWIT Transactions on State-of-the-art in Science and Engineering
PublisherWIT Press
Volume25
ISSN (Electronic)1755-8336

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