Direct numerical simulation of the diffusive convection and assessment of its impact on Artic [Arctic] climate change

This thesis focuses on the numerical modeling of the oceanic double-diffusive convection, an important small scale mixing process which is driven by the two orders of magnitude difference in diffusivities of heat and salt in seawater. This study explores the diffusive regime of double-diffusion whic...

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Bibliographic Details
Main Author: Prikasky, Ivo J.
Other Authors: Radko, Timour, Naval Postgraduate School (U.S.), Shaw, William
Format: Thesis
Language:unknown
Published: Monterey, California. Naval Postgraduate School 2007
Subjects:
Online Access:https://hdl.handle.net/10945/3247
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record_format openpolar
spelling ftnavalpschool:oai:calhoun.nps.edu:10945/3247 2024-06-09T07:43:51+00:00 Direct numerical simulation of the diffusive convection and assessment of its impact on Artic [Arctic] climate change Prikasky, Ivo J. Radko, Timour Naval Postgraduate School (U.S.) Shaw, William 2007-09 xiv, 65 p. : ill. application/pdf https://hdl.handle.net/10945/3247 unknown Monterey, California. Naval Postgraduate School 176914311 https://hdl.handle.net/10945/3247 Seawater Evolution Numerical analysis Meteorology Oceanography Climatology Mathematical models Climatic changes Thesis 2007 ftnavalpschool 2024-05-15T00:51:48Z This thesis focuses on the numerical modeling of the oceanic double-diffusive convection, an important small scale mixing process which is driven by the two orders of magnitude difference in diffusivities of heat and salt in seawater. This study explores the diffusive regime of double-diffusion which is realized when cold and fresh water overlies the warm and salty water. The aim of the research was to quantify the double diffusive transport in both smooth gradients and thermohaline staircases, and to develop clear insight into the origin of the staircases and specify conditions for their formation. Based on the numerical process modeling, it was determined that the evolutionary pattern of staircases is controlled by the merging events in which weak interfaces gradually erode and ultimately disappear. To illustrate dynamics of these events, a theoretical framework - merging theorem - has been developed. It was numerically confirmed that the merging theorem predicts the time scale of merging events within the order of magnitude. The validity of the lab derived 4/3 flux law was tested and it was determined that its form is consistent with the numerical results, but the amplitude requires adjustment. The computed fluxes from numerical experiments were comparable to the diffusive fluxes that were inferred from the Beaufort Gyre observations (Wilson, 2007) and an order of magnitude greater than the fluxes from earlier laboratory based experiments. Although a large discrepancy in the values of diffusive fluxes exists in the earlier laboratory and field studies, the present analysis suggests that the diffusive fluxes could play an important factor in the Arctic heat budget; hence, future study in this field is recommended. This study contributes to a better understanding of global climate change, which presents a new challenge to national security. The Navy has to be concerned with the impact of climate change on naval operations, specifically in the Arctic where the melting polar ice cap may soon provide a gateway ... Thesis Arctic Climate change Ice cap Polar Ice Cap Naval Postgraduate School: Calhoun Arctic
institution Open Polar
collection Naval Postgraduate School: Calhoun
op_collection_id ftnavalpschool
language unknown
topic Seawater
Evolution
Numerical analysis
Meteorology
Oceanography
Climatology
Mathematical models
Climatic changes
spellingShingle Seawater
Evolution
Numerical analysis
Meteorology
Oceanography
Climatology
Mathematical models
Climatic changes
Prikasky, Ivo J.
Direct numerical simulation of the diffusive convection and assessment of its impact on Artic [Arctic] climate change
topic_facet Seawater
Evolution
Numerical analysis
Meteorology
Oceanography
Climatology
Mathematical models
Climatic changes
description This thesis focuses on the numerical modeling of the oceanic double-diffusive convection, an important small scale mixing process which is driven by the two orders of magnitude difference in diffusivities of heat and salt in seawater. This study explores the diffusive regime of double-diffusion which is realized when cold and fresh water overlies the warm and salty water. The aim of the research was to quantify the double diffusive transport in both smooth gradients and thermohaline staircases, and to develop clear insight into the origin of the staircases and specify conditions for their formation. Based on the numerical process modeling, it was determined that the evolutionary pattern of staircases is controlled by the merging events in which weak interfaces gradually erode and ultimately disappear. To illustrate dynamics of these events, a theoretical framework - merging theorem - has been developed. It was numerically confirmed that the merging theorem predicts the time scale of merging events within the order of magnitude. The validity of the lab derived 4/3 flux law was tested and it was determined that its form is consistent with the numerical results, but the amplitude requires adjustment. The computed fluxes from numerical experiments were comparable to the diffusive fluxes that were inferred from the Beaufort Gyre observations (Wilson, 2007) and an order of magnitude greater than the fluxes from earlier laboratory based experiments. Although a large discrepancy in the values of diffusive fluxes exists in the earlier laboratory and field studies, the present analysis suggests that the diffusive fluxes could play an important factor in the Arctic heat budget; hence, future study in this field is recommended. This study contributes to a better understanding of global climate change, which presents a new challenge to national security. The Navy has to be concerned with the impact of climate change on naval operations, specifically in the Arctic where the melting polar ice cap may soon provide a gateway ...
author2 Radko, Timour
Naval Postgraduate School (U.S.)
Shaw, William
format Thesis
author Prikasky, Ivo J.
author_facet Prikasky, Ivo J.
author_sort Prikasky, Ivo J.
title Direct numerical simulation of the diffusive convection and assessment of its impact on Artic [Arctic] climate change
title_short Direct numerical simulation of the diffusive convection and assessment of its impact on Artic [Arctic] climate change
title_full Direct numerical simulation of the diffusive convection and assessment of its impact on Artic [Arctic] climate change
title_fullStr Direct numerical simulation of the diffusive convection and assessment of its impact on Artic [Arctic] climate change
title_full_unstemmed Direct numerical simulation of the diffusive convection and assessment of its impact on Artic [Arctic] climate change
title_sort direct numerical simulation of the diffusive convection and assessment of its impact on artic [arctic] climate change
publisher Monterey, California. Naval Postgraduate School
publishDate 2007
url https://hdl.handle.net/10945/3247
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
Ice cap
Polar Ice Cap
genre_facet Arctic
Climate change
Ice cap
Polar Ice Cap
op_relation 176914311
https://hdl.handle.net/10945/3247
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