Water Mass and Acoustic Analysis of the East Greenland Current.

Two cluster analysis techniques, one heuristic and one iterative, are used to investigate the spatial coherence of the water masses of the East Greenland Current (EGC), in the vicinity of the East Greenland Polar Front (EGPF). Both techniques are shown to be generally reliable, although the iterativ...

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Main Author: Clipson,James M
Other Authors: NAVAL POSTGRADUATE SCHOOL MONTEREY CA
Format: Text
Language:English
Published: 1986
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA175255
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA175255
id ftdtic:ADA175255
record_format openpolar
spelling ftdtic:ADA175255 2023-05-15T16:03:33+02:00 Water Mass and Acoustic Analysis of the East Greenland Current. Clipson,James M NAVAL POSTGRADUATE SCHOOL MONTEREY CA 1986-09 text/html http://www.dtic.mil/docs/citations/ADA175255 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA175255 en eng http://www.dtic.mil/docs/citations/ADA175255 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography *OCEAN CURRENTS *ACOUSTIC PROPERTIES SOURCES SPATIAL DISTRIBUTION WATER COHERENCE FORECASTING THESES VARIABLES SHALLOW WATER CLUSTERING PROFILES PATTERNS SEPARATION ACOUSTICS RANGE(DISTANCE) RAY TRACING ACOUSTIC VELOCITY NORTH ATLANTIC OCEAN WATER MASSES DEEP WATER BATHYTHERMOGRAPH DATA TRANSMISSION LOSS SONOBUOYS FRONTS(OCEANOGRAPHY) SOUND ANALYZERS East Greenland Current Acoustic Ducts Text 1986 ftdtic 2016-02-21T02:49:38Z Two cluster analysis techniques, one heuristic and one iterative, are used to investigate the spatial coherence of the water masses of the East Greenland Current (EGC), in the vicinity of the East Greenland Polar Front (EGPF). Both techniques are shown to be generally reliable, although the iterative technique is more consistent with classical oceanographic analyses. The techniques are applied to data to explore the grouping behavior of the water masses. They are also shown to have applications to multiple and single variable data. The cluster technique is shown to have applications in planning a sonobuoy pattern and in assessing the validity of XBT data prior to an acoustic forecast. Acoustic analysis shows that acoustic reciprocity does not hold for propagation in the waters of the EGC. Ranges from shallow to deep water are far in excess of those from deep to shallow water. Propagation across the EGPF is significantly different for normal and oblique cases. Propagation loss for oblique ranges is between 60 and 80 % of perpendicular ranges, mostly due to different source sound speed profiles. Three acoustic models, FACT, RAYMODE and PE are compared and contrasted. PE is found to be the most consistent and reliable, although both FACT and RAYMODE compare satisfactorily for propagation from shallow to deep water. For the reverse case, FACT overestimates ranges by a factor of two, whereas RAYMODE is exceedingly over optimistic in its forecast ranges. Keywords: Cluster analysis; Entity attribute; Separation distance; Ducting; Ray tracing. (Theses) Text East Greenland east greenland current Greenland North Atlantic Defense Technical Information Center: DTIC Technical Reports database Greenland
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Physical and Dynamic Oceanography
*OCEAN CURRENTS
*ACOUSTIC PROPERTIES
SOURCES
SPATIAL DISTRIBUTION
WATER
COHERENCE
FORECASTING
THESES
VARIABLES
SHALLOW WATER
CLUSTERING
PROFILES
PATTERNS
SEPARATION
ACOUSTICS
RANGE(DISTANCE)
RAY TRACING
ACOUSTIC VELOCITY
NORTH ATLANTIC OCEAN
WATER MASSES
DEEP WATER
BATHYTHERMOGRAPH DATA
TRANSMISSION LOSS
SONOBUOYS
FRONTS(OCEANOGRAPHY)
SOUND ANALYZERS
East Greenland Current
Acoustic Ducts
spellingShingle Physical and Dynamic Oceanography
*OCEAN CURRENTS
*ACOUSTIC PROPERTIES
SOURCES
SPATIAL DISTRIBUTION
WATER
COHERENCE
FORECASTING
THESES
VARIABLES
SHALLOW WATER
CLUSTERING
PROFILES
PATTERNS
SEPARATION
ACOUSTICS
RANGE(DISTANCE)
RAY TRACING
ACOUSTIC VELOCITY
NORTH ATLANTIC OCEAN
WATER MASSES
DEEP WATER
BATHYTHERMOGRAPH DATA
TRANSMISSION LOSS
SONOBUOYS
FRONTS(OCEANOGRAPHY)
SOUND ANALYZERS
East Greenland Current
Acoustic Ducts
Clipson,James M
Water Mass and Acoustic Analysis of the East Greenland Current.
topic_facet Physical and Dynamic Oceanography
*OCEAN CURRENTS
*ACOUSTIC PROPERTIES
SOURCES
SPATIAL DISTRIBUTION
WATER
COHERENCE
FORECASTING
THESES
VARIABLES
SHALLOW WATER
CLUSTERING
PROFILES
PATTERNS
SEPARATION
ACOUSTICS
RANGE(DISTANCE)
RAY TRACING
ACOUSTIC VELOCITY
NORTH ATLANTIC OCEAN
WATER MASSES
DEEP WATER
BATHYTHERMOGRAPH DATA
TRANSMISSION LOSS
SONOBUOYS
FRONTS(OCEANOGRAPHY)
SOUND ANALYZERS
East Greenland Current
Acoustic Ducts
description Two cluster analysis techniques, one heuristic and one iterative, are used to investigate the spatial coherence of the water masses of the East Greenland Current (EGC), in the vicinity of the East Greenland Polar Front (EGPF). Both techniques are shown to be generally reliable, although the iterative technique is more consistent with classical oceanographic analyses. The techniques are applied to data to explore the grouping behavior of the water masses. They are also shown to have applications to multiple and single variable data. The cluster technique is shown to have applications in planning a sonobuoy pattern and in assessing the validity of XBT data prior to an acoustic forecast. Acoustic analysis shows that acoustic reciprocity does not hold for propagation in the waters of the EGC. Ranges from shallow to deep water are far in excess of those from deep to shallow water. Propagation across the EGPF is significantly different for normal and oblique cases. Propagation loss for oblique ranges is between 60 and 80 % of perpendicular ranges, mostly due to different source sound speed profiles. Three acoustic models, FACT, RAYMODE and PE are compared and contrasted. PE is found to be the most consistent and reliable, although both FACT and RAYMODE compare satisfactorily for propagation from shallow to deep water. For the reverse case, FACT overestimates ranges by a factor of two, whereas RAYMODE is exceedingly over optimistic in its forecast ranges. Keywords: Cluster analysis; Entity attribute; Separation distance; Ducting; Ray tracing. (Theses)
author2 NAVAL POSTGRADUATE SCHOOL MONTEREY CA
format Text
author Clipson,James M
author_facet Clipson,James M
author_sort Clipson,James M
title Water Mass and Acoustic Analysis of the East Greenland Current.
title_short Water Mass and Acoustic Analysis of the East Greenland Current.
title_full Water Mass and Acoustic Analysis of the East Greenland Current.
title_fullStr Water Mass and Acoustic Analysis of the East Greenland Current.
title_full_unstemmed Water Mass and Acoustic Analysis of the East Greenland Current.
title_sort water mass and acoustic analysis of the east greenland current.
publishDate 1986
url http://www.dtic.mil/docs/citations/ADA175255
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA175255
geographic Greenland
geographic_facet Greenland
genre East Greenland
east greenland current
Greenland
North Atlantic
genre_facet East Greenland
east greenland current
Greenland
North Atlantic
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA175255
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766399228331950080