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Exchange flow between a canopy and open water

Published online by Cambridge University Press:  25 September 2008

MIRMOSADEGH JAMALI
Affiliation:
Department of Civil Engineering, Sharif University of Technology, Azadi Avenue, Teheran, Iran
XUEYAN ZHANG
Affiliation:
Department of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, Massachusetts, USA
HEIDI M. NEPF
Affiliation:
Department of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, Massachusetts, USA

Abstract

This paper theoretically and experimentally investigates the exchange flow due to temperature differences between open water and a canopy of aquatic plants. A numerical model is used to study the interfacial shape, frontal velocity and total volumetric exchange, and their dependence on a dimensionless vegetation drag parameter. The numerical predictions are consistent with the laboratory measurements. There is a short initial period in which the force balance is between buoyancy and inertia, followed by drag-dominated flow for which there is a balance between buoyancy and drag forces. After the initial stage, the gravity current propagating into the canopy takes a triangular shape whereas the current propagating into the open water has almost the classic unobstructed horizontal profile, but with a slowly decreasing depth. Near the edge of the canopy, but in the open region, the flow is found to be critical with a unit internal Froude number. The exchange flow rate and the front speed in the canopy decrease slowly with time whereas the gravity current in the open water has a constant speed. The magnitude of the exchange flow decreases as the canopy drag increases. Empirical equations for the flow properties are presented. A movie is available with the online version of the paper.

Type
Papers
Copyright
Copyright © Cambridge University Press 2008

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Jamali et al. supplementary movie

Movie 1. This animation shows the temporal evolution of lock-exchange flow in a half-canopy, corresponding to figure 5 in the paper. The vegetated area (initially containing cold water) is on the right-hand side, and the open water (initially containing warm water) on the left-hand side. The drag parameter (Cbar) is 13.2.

Download Jamali et al. supplementary movie(Video)
Video 3.6 MB