Chaotic advection and mixing in a western boundary current-recirculation system : laboratory experiments

Thesis (S.M.)--Joint Program in Oceanography (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), February 2001.

Bibliographic Details
Main Author: Deese, Heather E. (Heather Elizabeth), 1975-
Other Authors: Larry Pratt.
Format: Thesis
Language:eng
Published: Massachusetts Institute of Technology 2010
Subjects:
Online Access:http://hdl.handle.net/1721.1/53538
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author Deese, Heather E. (Heather Elizabeth), 1975-
author2 Larry Pratt.
author_facet Larry Pratt.
Deese, Heather E. (Heather Elizabeth), 1975-
author_sort Deese, Heather E. (Heather Elizabeth), 1975-
collection MIT
description Thesis (S.M.)--Joint Program in Oceanography (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), February 2001.
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spelling mit-1721.1/535382022-01-12T18:44:29Z Chaotic advection and mixing in a western boundary current-recirculation system : laboratory experiments Deese, Heather E. (Heather Elizabeth), 1975- Larry Pratt. Woods Hole Oceanographic Institution. Joint Program in Oceanography Massachusetts Institute of Technology. Dept. of Earth, Atmospheric, and Planetary Sciences. Woods Hole Oceanographic Institution. Massachusetts Institute of Technology. Department of Ocean Engineering Joint Program in Oceanography. Earth, Atmospheric, and Planetary Sciences. Woods Hole Oceanographic Institution. GC7.8 .D437 Oceanography Oceanic mixing Currents Thesis (S.M.)--Joint Program in Oceanography (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), February 2001. Includes bibliographical references (p. 116-118). I study the exchange between a boundary current and flanking horizontal recirculations in a 'sliced-cylinder' rotating tank laboratory experiment. Two flow configurations are investigated: a single recirculation and a double, figure-8, recirculation. The latter case involves a hyperbolic point, while the former does not. I investigate the stirring and mixing under both steady and unsteady forcing. I quantify the mixing in each case using effective diffusivity, Keff, and a corollary effective length, Leff, as derived by Nakamura (1995, 1996). This approach involves diagnosing the geometric complexity of a tracer field. Geometric complexity is indicative of advective stirring. Because stirring creates high gradients, flows with high advective stirring also have high diffusion, and stronger overall mixing. I calculate effective length from images of dye in the tank and find much higher values of Leff in the unsteady hyperbolic cases than in the other cases. Slight unsteadiness in flows involving hyperbolic points gives rise to a chaotic advection mechanism known as 'lobe dynamics'. These lobes carry fluid in and out of the recirculations, acting as extremely effective stirring mechanisms. I demonstrate the existence of these exchange lobes in the unsteady hyperbolic (figure-8) flow. The velocity field in the tank is calculated utilizing particle image velocimetry (PIV) techniques and a time series U(t) demonstrates the (forced) unsteadiness in the flow. Images of dye in the tank show exchange lobes forming at this same forcing period, and carrying fluid in and out of the recirculation. Based on the results of these experiments, I am able to confirm that, at least in this controlled environment, basic geometry has a profound effect on the mixing effectiveness of a recirculation. I demonstrate radically increased stirring and mixing in the unsteady hyperbolic flow as compared to steady flows and flows without hyperbolic points. Recirculations are ubiquitous in the world ocean; they occur on a variety of scales, in many different configurations, and at all depths. Some of these configurations involve hyperbolic points, while others do not. Chaotic advection via lobe exchange may be an important component of the mixing at multiple locations in the ocean where hyperbolic recirculation geometries exist. by Heather E. Deese. S.M. 2010-04-07T13:38:28Z 2010-04-07T13:38:28Z 2001 Thesis http://hdl.handle.net/1721.1/53538 47784764 eng M.I.T. theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. See provided URL for inquiries about permission. http://dspace.mit.edu/handle/1721.1/7582 118 p. application/pdf Massachusetts Institute of Technology
spellingShingle Joint Program in Oceanography.
Earth, Atmospheric, and Planetary Sciences.
Woods Hole Oceanographic Institution.
GC7.8 .D437
Oceanography
Oceanic mixing
Currents
Deese, Heather E. (Heather Elizabeth), 1975-
Chaotic advection and mixing in a western boundary current-recirculation system : laboratory experiments
title Chaotic advection and mixing in a western boundary current-recirculation system : laboratory experiments
title_full Chaotic advection and mixing in a western boundary current-recirculation system : laboratory experiments
title_fullStr Chaotic advection and mixing in a western boundary current-recirculation system : laboratory experiments
title_full_unstemmed Chaotic advection and mixing in a western boundary current-recirculation system : laboratory experiments
title_short Chaotic advection and mixing in a western boundary current-recirculation system : laboratory experiments
title_sort chaotic advection and mixing in a western boundary current recirculation system laboratory experiments
topic Joint Program in Oceanography.
Earth, Atmospheric, and Planetary Sciences.
Woods Hole Oceanographic Institution.
GC7.8 .D437
Oceanography
Oceanic mixing
Currents
url http://hdl.handle.net/1721.1/53538
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