Surface Forcing of Potential Vorticity in a Numerical Model
Mode water formation has long been treated as a buoyancy flux problem; however this approach fails to explain all of the variability of mode water. A number of different approaches have been demonstrated to explain more of this variability, such as links to North Atlantic Oscillation and the Gulf St...
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ftfloridastunidc:oai:fsu.digital.flvc.org:fsu_175746 2023-05-15T17:33:48+02:00 Surface Forcing of Potential Vorticity in a Numerical Model Beck, Michael (authoraut) Dewar, William (professor directing thesis) Krishnamurti, Ruby (committee member) Chanton, Jeff (committee member) Department of Earth, Ocean and Atmospheric Sciences (degree granting department) Florida State University (degree granting institution) 1 online resource computer application/pdf http://purl.flvc.org/fsu/fd/FSU_migr_etd-1188 http://fsu.digital.flvc.org/islandora/object/fsu%3A175746/datastream/TN/view/Surface%20Forcing%20of%20Potential%20Vorticity%20in%20a%20Numerical%20Model.jpg English eng eng Florida State University This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s). The copyright in theses and dissertations completed at Florida State University is held by the students who author them. Oceanography Text ftfloridastunidc 2020-08-10T21:04:17Z Mode water formation has long been treated as a buoyancy flux problem; however this approach fails to explain all of the variability of mode water. A number of different approaches have been demonstrated to explain more of this variability, such as links to North Atlantic Oscillation and the Gulf Stream position. These help to add to knowledge of mode water but it is still poorly understood. According to the impermeability theorem, the potential vorticity should be largely driven at the surface. In addition to this we take new approach to PV surface forcing suggested by Thomas that the PV loss is due to both buoyancy and momentum flux at the surface. The question of the relative roles of these two processes within a numerical model is addressed. It is determined that for the models mode water the buoyancy flux is the dominant cause of PV loss from the ocean and is roughly 4 times greater in magnitude that the momentum flux in the mean. A Thesis Submitted to the Department of Oceanography in Partial Fulfillment of the Requirements for the Degree of Master of Science. Summer Semester, 2008. May 20, 2008. Surface Forcing, Momentum Flux, Buoyancy Flux, Potential Vorticity Includes bibliographical references. William Dewar, Professor Directing Thesis; Ruby Krishnamurti, Committee Member; Jeff Chanton, Committee Member. Text North Atlantic North Atlantic oscillation Florida State University Digital Library (FSUDL) Dewar ENVELOPE(-21.158,-21.158,-80.534,-80.534) |
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Florida State University Digital Library (FSUDL) |
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ftfloridastunidc |
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English |
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Oceanography |
spellingShingle |
Oceanography Surface Forcing of Potential Vorticity in a Numerical Model |
topic_facet |
Oceanography |
description |
Mode water formation has long been treated as a buoyancy flux problem; however this approach fails to explain all of the variability of mode water. A number of different approaches have been demonstrated to explain more of this variability, such as links to North Atlantic Oscillation and the Gulf Stream position. These help to add to knowledge of mode water but it is still poorly understood. According to the impermeability theorem, the potential vorticity should be largely driven at the surface. In addition to this we take new approach to PV surface forcing suggested by Thomas that the PV loss is due to both buoyancy and momentum flux at the surface. The question of the relative roles of these two processes within a numerical model is addressed. It is determined that for the models mode water the buoyancy flux is the dominant cause of PV loss from the ocean and is roughly 4 times greater in magnitude that the momentum flux in the mean. A Thesis Submitted to the Department of Oceanography in Partial Fulfillment of the Requirements for the Degree of Master of Science. Summer Semester, 2008. May 20, 2008. Surface Forcing, Momentum Flux, Buoyancy Flux, Potential Vorticity Includes bibliographical references. William Dewar, Professor Directing Thesis; Ruby Krishnamurti, Committee Member; Jeff Chanton, Committee Member. |
author2 |
Beck, Michael (authoraut) Dewar, William (professor directing thesis) Krishnamurti, Ruby (committee member) Chanton, Jeff (committee member) Department of Earth, Ocean and Atmospheric Sciences (degree granting department) Florida State University (degree granting institution) |
format |
Text |
title |
Surface Forcing of Potential Vorticity in a Numerical Model |
title_short |
Surface Forcing of Potential Vorticity in a Numerical Model |
title_full |
Surface Forcing of Potential Vorticity in a Numerical Model |
title_fullStr |
Surface Forcing of Potential Vorticity in a Numerical Model |
title_full_unstemmed |
Surface Forcing of Potential Vorticity in a Numerical Model |
title_sort |
surface forcing of potential vorticity in a numerical model |
publisher |
Florida State University |
url |
http://purl.flvc.org/fsu/fd/FSU_migr_etd-1188 http://fsu.digital.flvc.org/islandora/object/fsu%3A175746/datastream/TN/view/Surface%20Forcing%20of%20Potential%20Vorticity%20in%20a%20Numerical%20Model.jpg |
long_lat |
ENVELOPE(-21.158,-21.158,-80.534,-80.534) |
geographic |
Dewar |
geographic_facet |
Dewar |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_rights |
This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s). The copyright in theses and dissertations completed at Florida State University is held by the students who author them. |
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