Linear and nonlinear stratified spindown over sloping topography

Thesis (Ph. D.)--Joint Program in Oceanography/Applied Ocean Science and Engineering (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), 2010.

Bibliographic Details
Main Author: Benthuysen, Jessica A
Other Authors: Steven J. Lentz and Leif N. Thomas.
Format: Thesis
Language:eng
Published: Massachusetts Institute of Technology 2010
Subjects:
Online Access:http://hdl.handle.net/1721.1/59740
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author Benthuysen, Jessica A
author2 Steven J. Lentz and Leif N. Thomas.
author_facet Steven J. Lentz and Leif N. Thomas.
Benthuysen, Jessica A
author_sort Benthuysen, Jessica A
collection MIT
description Thesis (Ph. D.)--Joint Program in Oceanography/Applied Ocean Science and Engineering (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), 2010.
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spelling mit-1721.1/597402022-01-13T21:52:28Z Linear and nonlinear stratified spindown over sloping topography Benthuysen, Jessica A Steven J. Lentz and Leif N. Thomas. Woods Hole Oceanographic Institution. Joint Program in Oceanography/Applied Ocean Science and Engineering Woods Hole Oceanographic Institution Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences Joint Program in Oceanography/Applied Ocean Science and Engineering. Earth, Atmospheric, and Planetary Sciences. Woods Hole Oceanographic Institution. Ocean currents Ocean circulation Thesis (Ph. D.)--Joint Program in Oceanography/Applied Ocean Science and Engineering (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), 2010. Cataloged from PDF version of thesis. Includes bibliographical references (p. 199-205). In a stratified rotating fluid, frictionally driven circulations couple with the buoyancy field over sloping topography. Analytical and numerical methods are used to quantify the impact of this coupling on the vertical circulation, spindown of geostrophic flows, and the formation of a shelfbreak jet. Over a stratified. slope, linear spindown of a geostrophic along-isobath flow induces cross-isobath Ekman flows. Ekman advection of buoyancy weakens the vertical circulation and slows spindown. Upslope (downslope) Ekman flows tend to inject (remove) potential vorticity into (from) the ocean. Momentum advection and nonlinear buoyancy advection are examined in setting asymmetries in the vertical circulation and the vertical relative vorticity field. During nonlinear homogeneous spindown over a flat bottom, momentum advection weakens Ekman pumping and strengthens Ekman suction, while cyclonic vorticity decays faster than anticyclonic vorticity. During nonlinear stratified spindown over a slope, nonlinear advection of buoyancy enhances the asymmetry in Ekman pumping and suction, whereas anticyclonic vorticity can decay faster than cyclonic vorticity outside of the boundary layers. During the adjustment of a spatially uniform geostrophic current over a shelfbreak, coupling between the Ekman flow and the buoyancy field generates Ekman pumping near the shelfbreak, which leads to the formation of a jet. Scalings are presented for the upwelling strength, the length scale over which it occurs, and the timescale for jet formation. The results are applied to the Middle Atlantic Bight shelfbreak. by Jessica A. Benthuysen. Ph.D. 2010-10-29T18:28:18Z 2010-10-29T18:28:18Z 2010 2010 Thesis http://hdl.handle.net/1721.1/59740 670428770 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 205 p. application/pdf Massachusetts Institute of Technology
spellingShingle Joint Program in Oceanography/Applied Ocean Science and Engineering.
Earth, Atmospheric, and Planetary Sciences.
Woods Hole Oceanographic Institution.
Ocean currents
Ocean circulation
Benthuysen, Jessica A
Linear and nonlinear stratified spindown over sloping topography
title Linear and nonlinear stratified spindown over sloping topography
title_full Linear and nonlinear stratified spindown over sloping topography
title_fullStr Linear and nonlinear stratified spindown over sloping topography
title_full_unstemmed Linear and nonlinear stratified spindown over sloping topography
title_short Linear and nonlinear stratified spindown over sloping topography
title_sort linear and nonlinear stratified spindown over sloping topography
topic Joint Program in Oceanography/Applied Ocean Science and Engineering.
Earth, Atmospheric, and Planetary Sciences.
Woods Hole Oceanographic Institution.
Ocean currents
Ocean circulation
url http://hdl.handle.net/1721.1/59740
work_keys_str_mv AT benthuysenjessicaa linearandnonlinearstratifiedspindownoverslopingtopography