Mixed layer dynamics in the onset of freezing

A two layer ocean mixed layer model is used to study the relationship between onset of freezing and mixed layer depth, wind forcing, surface buoyancy flux, and temperature and salinity changes between the two layers. Universal non- dimensional parameters for stability and surface forcing are derived...

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Main Author: Claes, Dennis C.
Other Authors: Garwood, Roland W., Naval Postgraduate School (U.S.), Oceanography, Davidson, Kenneth L.
Format: Thesis
Language:English
Published: Monterey, California: Naval Postgraduate School 1990
Subjects:
Online Access:https://hdl.handle.net/10945/27565
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record_format openpolar
spelling ftnavalpschool:oai:calhoun.nps.edu:10945/27565 2024-06-09T07:49:30+00:00 Mixed layer dynamics in the onset of freezing Claes, Dennis C. Garwood, Roland W. Naval Postgraduate School (U.S.) Oceanography Davidson, Kenneth L. 1990-12 viii, 101 p. application/pdf https://hdl.handle.net/10945/27565 en_US eng Monterey, California: Naval Postgraduate School https://hdl.handle.net/10945/27565 This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States. Oceanography sea ice mixed layer modeling freezing Dynamics Temperature Thesis 1990 ftnavalpschool 2024-05-15T00:46:59Z A two layer ocean mixed layer model is used to study the relationship between onset of freezing and mixed layer depth, wind forcing, surface buoyancy flux, and temperature and salinity changes between the two layers. Universal non- dimensional parameters for stability and surface forcing are derived and related to the maximum freezing rate. Analytic solutions to the model are found in terms of the universal parameters and the model turbulent mixing tuning constants. Sensitivity studies show the dependence of the freezing rate on the stability as defined by the salinity and temperature jumps, the forcing by wind stress and surface heat flux, and the mixed layer depth. Results show that an increase in heat flux produces a nearly linear increase in the freezing rate. Mixing energy from the wind, proportional to the wind speed cubed, results in a nearly linear decrease in freezing rate. There is a nonlinear relationship between the temperature jump between layers and the freezing rate. Warming of the deeper layer decreases the freezing rate and ultimately prevents freezing. A nonlinear relation was also found between the salinity jump and freezing rate. Increase in the deeper layer salinity causes an increase in the freezing rate and leads to the maximum expected freezing rate. A nearly hyperbolic relationship between the mixed layer depth and freezing rate was found. As the mixed layer depth increases from near zero, the freezing rate increases rapidly and then the maximum expected freezing rate is approached asymptotically. Approved for public release; distribution is unlimited. Lieutenant Commander, United States Navy http://archive.org/details/mixedlayerdynami1094527565 Thesis Sea ice Naval Postgraduate School: Calhoun
institution Open Polar
collection Naval Postgraduate School: Calhoun
op_collection_id ftnavalpschool
language English
topic Oceanography
sea ice
mixed layer modeling
freezing
Dynamics
Temperature
spellingShingle Oceanography
sea ice
mixed layer modeling
freezing
Dynamics
Temperature
Claes, Dennis C.
Mixed layer dynamics in the onset of freezing
topic_facet Oceanography
sea ice
mixed layer modeling
freezing
Dynamics
Temperature
description A two layer ocean mixed layer model is used to study the relationship between onset of freezing and mixed layer depth, wind forcing, surface buoyancy flux, and temperature and salinity changes between the two layers. Universal non- dimensional parameters for stability and surface forcing are derived and related to the maximum freezing rate. Analytic solutions to the model are found in terms of the universal parameters and the model turbulent mixing tuning constants. Sensitivity studies show the dependence of the freezing rate on the stability as defined by the salinity and temperature jumps, the forcing by wind stress and surface heat flux, and the mixed layer depth. Results show that an increase in heat flux produces a nearly linear increase in the freezing rate. Mixing energy from the wind, proportional to the wind speed cubed, results in a nearly linear decrease in freezing rate. There is a nonlinear relationship between the temperature jump between layers and the freezing rate. Warming of the deeper layer decreases the freezing rate and ultimately prevents freezing. A nonlinear relation was also found between the salinity jump and freezing rate. Increase in the deeper layer salinity causes an increase in the freezing rate and leads to the maximum expected freezing rate. A nearly hyperbolic relationship between the mixed layer depth and freezing rate was found. As the mixed layer depth increases from near zero, the freezing rate increases rapidly and then the maximum expected freezing rate is approached asymptotically. Approved for public release; distribution is unlimited. Lieutenant Commander, United States Navy http://archive.org/details/mixedlayerdynami1094527565
author2 Garwood, Roland W.
Naval Postgraduate School (U.S.)
Oceanography
Davidson, Kenneth L.
format Thesis
author Claes, Dennis C.
author_facet Claes, Dennis C.
author_sort Claes, Dennis C.
title Mixed layer dynamics in the onset of freezing
title_short Mixed layer dynamics in the onset of freezing
title_full Mixed layer dynamics in the onset of freezing
title_fullStr Mixed layer dynamics in the onset of freezing
title_full_unstemmed Mixed layer dynamics in the onset of freezing
title_sort mixed layer dynamics in the onset of freezing
publisher Monterey, California: Naval Postgraduate School
publishDate 1990
url https://hdl.handle.net/10945/27565
genre Sea ice
genre_facet Sea ice
op_relation https://hdl.handle.net/10945/27565
op_rights This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States.
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