Momentum exchange near ice keels in the under ice ocean boundary layer

This thesis describes momentum exchange in the under-ice ocean boundary layer near ice keels. Understanding ice-ocean momentum exchange is important for accurate predictive ice modeling. Due to climate change, increased naval presence in the Arctic region is anticipated and ice models will become ne...

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Bibliographic Details
Main Author: Bleidorn, John Charles.
Other Authors: Stanton, Timothy, Naval Postgraduate School (U.S.), Shaw, William.
Format: Thesis
Language:unknown
Published: Monterey, California. Naval Postgraduate School 2008
Subjects:
Online Access:https://hdl.handle.net/10945/4282
id ftnavalpschool:oai:calhoun.nps.edu:10945/4282
record_format openpolar
spelling ftnavalpschool:oai:calhoun.nps.edu:10945/4282 2024-06-09T07:43:37+00:00 Momentum exchange near ice keels in the under ice ocean boundary layer Bleidorn, John Charles. Stanton, Timothy Naval Postgraduate School (U.S.) Shaw, William. 2008-03 xii, 37 p. : ill. application/pdf https://hdl.handle.net/10945/4282 unknown Monterey, California. Naval Postgraduate School 226967949 https://hdl.handle.net/10945/4282 Momentum transfer Sea ice drift Arctic Ocean Mathematical models Boundary layer (Meteorology) Arctic regions Turbulent boundary layer Thesis 2008 ftnavalpschool 2024-05-15T00:24:02Z This thesis describes momentum exchange in the under-ice ocean boundary layer near ice keels. Understanding ice-ocean momentum exchange is important for accurate predictive ice modeling. Due to climate change, increased naval presence in the Arctic region is anticipated and ice models will become necessary for tactical and safety reasons. Measurements took place in March 2007 in the Beaufort Sea at the Applied Physics Laboratory Ice Station sponsored by the U.S. Navy. Turbulence measurements were made at a single point behind a large multi-year ice ridge in the upper ocean boundary layer. The keel was found to be at least 12.5m deep and much broader than expected. Ocean profiles showed the pycnocline between 13-18m deep and thus a unique situation of measuring the flow around a large ice structure in a shallow boundary layer presented itself. Results indicate that estimates of turbulence intensity depend on ice speed, direction and measurement depth. Velocity spectra indicate periods of low inertial subrange levels likely resulting from close proximity to the pycnocline. Low frequency variance in the velocity spectra was also observed and is thought to be a wake effect resulting from an under ice structure upstream of the flow. Approved for public release; distribution is unlimited. US Navy (USN) author. http://archive.org/details/momentumexchange109454282 Thesis Arctic Arctic Ocean Beaufort Sea Climate change Sea ice Naval Postgraduate School: Calhoun Arctic Arctic Ocean
institution Open Polar
collection Naval Postgraduate School: Calhoun
op_collection_id ftnavalpschool
language unknown
topic Momentum transfer
Sea ice drift
Arctic Ocean
Mathematical models
Boundary layer (Meteorology)
Arctic regions
Turbulent boundary layer
spellingShingle Momentum transfer
Sea ice drift
Arctic Ocean
Mathematical models
Boundary layer (Meteorology)
Arctic regions
Turbulent boundary layer
Bleidorn, John Charles.
Momentum exchange near ice keels in the under ice ocean boundary layer
topic_facet Momentum transfer
Sea ice drift
Arctic Ocean
Mathematical models
Boundary layer (Meteorology)
Arctic regions
Turbulent boundary layer
description This thesis describes momentum exchange in the under-ice ocean boundary layer near ice keels. Understanding ice-ocean momentum exchange is important for accurate predictive ice modeling. Due to climate change, increased naval presence in the Arctic region is anticipated and ice models will become necessary for tactical and safety reasons. Measurements took place in March 2007 in the Beaufort Sea at the Applied Physics Laboratory Ice Station sponsored by the U.S. Navy. Turbulence measurements were made at a single point behind a large multi-year ice ridge in the upper ocean boundary layer. The keel was found to be at least 12.5m deep and much broader than expected. Ocean profiles showed the pycnocline between 13-18m deep and thus a unique situation of measuring the flow around a large ice structure in a shallow boundary layer presented itself. Results indicate that estimates of turbulence intensity depend on ice speed, direction and measurement depth. Velocity spectra indicate periods of low inertial subrange levels likely resulting from close proximity to the pycnocline. Low frequency variance in the velocity spectra was also observed and is thought to be a wake effect resulting from an under ice structure upstream of the flow. Approved for public release; distribution is unlimited. US Navy (USN) author. http://archive.org/details/momentumexchange109454282
author2 Stanton, Timothy
Naval Postgraduate School (U.S.)
Shaw, William.
format Thesis
author Bleidorn, John Charles.
author_facet Bleidorn, John Charles.
author_sort Bleidorn, John Charles.
title Momentum exchange near ice keels in the under ice ocean boundary layer
title_short Momentum exchange near ice keels in the under ice ocean boundary layer
title_full Momentum exchange near ice keels in the under ice ocean boundary layer
title_fullStr Momentum exchange near ice keels in the under ice ocean boundary layer
title_full_unstemmed Momentum exchange near ice keels in the under ice ocean boundary layer
title_sort momentum exchange near ice keels in the under ice ocean boundary layer
publisher Monterey, California. Naval Postgraduate School
publishDate 2008
url https://hdl.handle.net/10945/4282
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Beaufort Sea
Climate change
Sea ice
genre_facet Arctic
Arctic Ocean
Beaufort Sea
Climate change
Sea ice
op_relation 226967949
https://hdl.handle.net/10945/4282
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