dc.contributor.author Steinmoeller, Derek dc.date.accessioned 2009-05-15 19:55:24 (GMT) dc.date.available 2009-05-15 19:55:24 (GMT) dc.date.issued 2009-05-15T19:55:24Z dc.date.submitted 2009 dc.identifier.uri http://hdl.handle.net/10012/4417 dc.description.abstract In non-rotating fluids, boundary-layer separation occurs when the nearly inviscid flow just outside a viscous boundary-layer experiences an appreciable deceleration due to a region of adverse pressure gradient. The fluid ceases to flow along the boundary due to a flow recirculation region close to the boundary. The flow is then said to be "detached." en In recent decades, attention has shifted to the study of boundary-layer separation in a rotating reference frame due to its significance in Geophysical Fluid Dynamics (GFD). Since the Earth is a rotating sphere, the so-called β-plane approximation f = f0 + βy is often used to account for the inherent meridional variation of the Coriolis parameter, f, while still solving the governing equations on a plane. Numerical simulations of currents on the β-plane have been useful in understanding ocean currents such as the Gulf Stream, the Brazil Current, and the Antarctic Circumpolar Current to name a few. In this thesis, we first consider the problem of prograde flow past a cylindrical obstacle on the β-plane. The problem is governed by the barotropic vorticity equation and is solved using a numerical method that is a combination of a finite difference method and a spectral method. A modified form of the β-plane approximation is proposed to avoid computational difficulties. Results are given and discussed for flow past a circular cylinder at selected Reynolds numbers (Re) and non-dimensional β-parameters (β^). Results are then given and discussed for flow past an elliptic cylinder of a fixed aspect ratio (r = 0.2) and at two angles of inclination (90°, 15°) at selected Re and β^. In general, it is found that the β-effect acts to suppress boundary-layer separation and to allow Rossby waves to form in the exterior flow field. In the asymmetrical case of an inclined elliptic cylinder, the β-effect was found to constrain the region of vortex shedding to a small region near the trailing edge of the cylinder. The shed vortices were found to propagate around the trailing edge instead of in the expected downstream direction, as observed in the non-rotating case. The second problem considered in this thesis is the separation of western boundary currents from a curved coastline. This problem is also governed by the barotropic vorticity equation, and it is solved on an idealized model domain suitable for investigating the effects that boundary curvature has on the tendency of a boundary current to separate. The numerical method employed is a two-dimensional Chebyshev spectral collocation method and yields high order accuracy that helps to better resolve the boundary-layer dynamics in comparison to low-order methods. Results are given for a selection of boundary curvatures, non-dimensional β-parameters (β^), Reynolds numbers (Re), and Munk Numbers (Mu). In general, it is found than an increase in β^ will act to suppress boundary-layer separation. However, a sufficiently sharp obstacle can overcome the β-effect and force the boundary current to separate regardless of the value of β^. It is also found that in the inertial limit (small Mu, large Re) the flow region to the east of the primary boundary current is dominated by strong wave interactions and large eddies which form as a result of shear instabilities. In an interesting case of the inertial limit, strong waves were found to interact with the separation region, causing it to expand and propagate to the east as a large eddy. This idealized the mechanism by which western boundary currents such as the Gulf Stream generate eddies in the world's oceans. dc.language.iso en en dc.publisher University of Waterloo en dc.subject beta-plane en dc.subject fluid dynamics en dc.subject barotropic en dc.subject vorticity en dc.subject flow en dc.subject geophysical fluid en dc.subject ocean en dc.subject current en dc.subject boundary en dc.subject layer en dc.subject separation en dc.subject geostrophy en dc.subject quasi-geostrophy en dc.subject cylinder en dc.subject cape hatteras en dc.subject gulf stream en dc.subject western boundary current en dc.subject viscous en dc.subject rotating en dc.subject rotation en dc.subject GFD en dc.subject CFD en dc.subject Chebyshev en dc.subject Fourier en dc.subject spectral en dc.subject numerics en dc.subject influence matrix en dc.subject earth en dc.subject eddy en dc.subject Rossby en dc.subject vortex en dc.subject wave en dc.subject vortices en dc.subject eddies en dc.subject cylindrical en dc.subject obstacle en dc.title Flow Separation on the β-plane en dc.type Master Thesis en dc.pending false en dc.subject.program Applied Mathematics en uws-etd.degree.department Applied Mathematics en uws-etd.degree Master of Mathematics en uws.typeOfResource Text en uws.peerReviewStatus Unreviewed en uws.scholarLevel Graduate en
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