Identification of acoustically active Arctic pressure ridges through the use of RADARSAT Geophysical Processor System (RGPS) sea ice products

The identification of acoustically active pressure ridges in the Arctic Ocean represents an important step in the development of a physics based, operational Polar ambient noise model. One method to accomplish this goal is through the use of satellite based remote sensors, specifically synthetic ape...

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Main Author: Speckhahn, Marcus M.
Other Authors: Bourke, Robert H., Wilson, James H., Guest, Peter S.
Format: Thesis
Language:English
Published: Monterey, California. Naval Postgraduate School 1998
Subjects:
Online Access:https://hdl.handle.net/10945/8487
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record_format openpolar
spelling ftnavalpschool:oai:calhoun.nps.edu:10945/8487 2024-06-09T07:43:41+00:00 Identification of acoustically active Arctic pressure ridges through the use of RADARSAT Geophysical Processor System (RGPS) sea ice products Speckhahn, Marcus M. Bourke, Robert H. Wilson, James H. Guest, Peter S. 1998-06 xxv, 306 p.;28 cm. application/pdf https://hdl.handle.net/10945/8487 en_US eng Monterey, California. Naval Postgraduate School https://hdl.handle.net/10945/8487 Polar Oceanography RADARSAT Geophysical Processor System Low Frequency Ambient Noise Thesis 1998 ftnavalpschool 2024-05-15T00:28:56Z The identification of acoustically active pressure ridges in the Arctic Ocean represents an important step in the development of a physics based, operational Polar ambient noise model. One method to accomplish this goal is through the use of satellite based remote sensors, specifically synthetic aperture radar (SAR). A proof of concept study was conducted that determined that the RADARSAT Geophysical Processor System (RGPS) produces SAR derived sea ice products capable of quantifying large scale ice deformation that may produce significant levels of low frequency ambient noise. This research also identifies the meteorological forcing that causes the sequence of divergent and convergent events in the ice cover, which results in the creation of open water leads and subsequent generation of noisy pressure ridges. Offshore followed by onshore winds near coasts and land fast ice and atmospheric lows/troughs followed by atmospheric highs/ridges or velocity shear in straight isobaric flow result in significant pressure ridge formation. The RGPS ridging algorithm shows that more ridges exist in RGPS cells exhibiting large cell area changes than in those with small area changes, assuming relatively constant cell heights in all cells. The feasibility of using ice divergence fields generated by Fleet Numerical Meteorology and Oceanography Center's (FNMOC's) Polar Ice Prediction System (PIPS) was evaluated. PIPS modeled ice divergence patterns reasonably well, although divergence values in the high Arctic ice cover were underestimated Approved for public release; distribution is unlimited. U.S. Navy (U.S.N.) author. http://archive.org/details/identificationof109458487 Thesis Arctic Arctic Ocean Sea ice Naval Postgraduate School: Calhoun Arctic Arctic Ocean
institution Open Polar
collection Naval Postgraduate School: Calhoun
op_collection_id ftnavalpschool
language English
topic Polar Oceanography
RADARSAT Geophysical Processor System
Low Frequency Ambient Noise
spellingShingle Polar Oceanography
RADARSAT Geophysical Processor System
Low Frequency Ambient Noise
Speckhahn, Marcus M.
Identification of acoustically active Arctic pressure ridges through the use of RADARSAT Geophysical Processor System (RGPS) sea ice products
topic_facet Polar Oceanography
RADARSAT Geophysical Processor System
Low Frequency Ambient Noise
description The identification of acoustically active pressure ridges in the Arctic Ocean represents an important step in the development of a physics based, operational Polar ambient noise model. One method to accomplish this goal is through the use of satellite based remote sensors, specifically synthetic aperture radar (SAR). A proof of concept study was conducted that determined that the RADARSAT Geophysical Processor System (RGPS) produces SAR derived sea ice products capable of quantifying large scale ice deformation that may produce significant levels of low frequency ambient noise. This research also identifies the meteorological forcing that causes the sequence of divergent and convergent events in the ice cover, which results in the creation of open water leads and subsequent generation of noisy pressure ridges. Offshore followed by onshore winds near coasts and land fast ice and atmospheric lows/troughs followed by atmospheric highs/ridges or velocity shear in straight isobaric flow result in significant pressure ridge formation. The RGPS ridging algorithm shows that more ridges exist in RGPS cells exhibiting large cell area changes than in those with small area changes, assuming relatively constant cell heights in all cells. The feasibility of using ice divergence fields generated by Fleet Numerical Meteorology and Oceanography Center's (FNMOC's) Polar Ice Prediction System (PIPS) was evaluated. PIPS modeled ice divergence patterns reasonably well, although divergence values in the high Arctic ice cover were underestimated Approved for public release; distribution is unlimited. U.S. Navy (U.S.N.) author. http://archive.org/details/identificationof109458487
author2 Bourke, Robert H.
Wilson, James H.
Guest, Peter S.
format Thesis
author Speckhahn, Marcus M.
author_facet Speckhahn, Marcus M.
author_sort Speckhahn, Marcus M.
title Identification of acoustically active Arctic pressure ridges through the use of RADARSAT Geophysical Processor System (RGPS) sea ice products
title_short Identification of acoustically active Arctic pressure ridges through the use of RADARSAT Geophysical Processor System (RGPS) sea ice products
title_full Identification of acoustically active Arctic pressure ridges through the use of RADARSAT Geophysical Processor System (RGPS) sea ice products
title_fullStr Identification of acoustically active Arctic pressure ridges through the use of RADARSAT Geophysical Processor System (RGPS) sea ice products
title_full_unstemmed Identification of acoustically active Arctic pressure ridges through the use of RADARSAT Geophysical Processor System (RGPS) sea ice products
title_sort identification of acoustically active arctic pressure ridges through the use of radarsat geophysical processor system (rgps) sea ice products
publisher Monterey, California. Naval Postgraduate School
publishDate 1998
url https://hdl.handle.net/10945/8487
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
genre_facet Arctic
Arctic Ocean
Sea ice
op_relation https://hdl.handle.net/10945/8487
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