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Massachusetts Institute of Technology

Mechanisms of turbulent mixing in the Continental Shelf bottom boundary layer

Abstract

dc:description.abstract

The bottom boundary layer is an important dynamical region of shallow water flows. In this thesis, the problem of turbulent mixing in the coastal bottom boundary layer is investigated with a unique set of field measurements of velocity and sound speed that span a significant fraction of the boundary layer obtained over a six-week long period in the late summer of 1996 on the New England shelf. The energetics of the turbulent fluctuations are investigated by testing simplified budgets for turbulent kinetic energy and scalar variance. The turbulent kinetic energy budget is locally balanced while the scalar variance budget is not, probably due to turbulent diffusion. The direct effects of stratification are consistently significant only in the outer part of the boundary layer, where the flux Richardson number is approximately equal to a critical value of 0.2. Turbulence closure is investigated in terms of non-dimensional profiles of velocity and sound speed. Close to the bottom, the results are consistent with Monin-Obukhov similarity theory, while in the outer part of the boundary layer other scales including the height of the boundary layer are important for setting the turbulent length scale.

Degree

thesis:*
Department dc:contributor.department
Joint Program in Oceanography
Grantor dc:publisher
Massachusetts Institute of Technology
Year dc:date.issued
2000

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Shaw, William J. (William James), 1971-
Advisor dc:contributor.advisor
  • John H. Trowbridge.

Subjects

dc:subject × 3

Rights

dc:rights
Statement dc:rights
  • 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.
Language dc:language.iso
eng

Identifiers

dc:identifier.*
Handle dc:identifier.uri
http://hdl.handle.net/1721.1/58518
OAI identifier oai:identifier
oai:dspace.mit.edu:1721.1/58518

Chain of custody

source
Harvested from
MIT
Base URL
dspace.mit.edu/oai/request
Last updated
2026-07-22
Source record
OAI-PMH GetRecord
citation

Shaw, William J. (William James), 1971-. Mechanisms of turbulent mixing in the Continental Shelf bottom boundary layer. Massachusetts Institute of Technology, 2000. http://hdl.handle.net/1721.1/58518