The Reflection of Low Frequency Sonar Signals from a Smooth Ocean Bottom. Part I. Experimental Reflection Losses at Locations off the California Coast and in the Bering Sea

Underwater acoustic tests in three different areas are discussed: Area I is in 200-fathom water while Areas II and III are deep-water, 2000-fathom areas. From the data obtained bottom reflection losses were computed as a function of grazing angle for low frequency, 0.7 to 3.0 kc sound pulses. Measur...

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Bibliographic Details
Main Authors: Whitney,J A, Yee,G S, Gardner,R R
Other Authors: NAVY ELECTRONICS LAB SAN DIEGO CA
Format: Text
Language:English
Published: 1963
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA074407
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA074407
id ftdtic:ADA074407
record_format openpolar
spelling ftdtic:ADA074407 2023-05-15T15:43:29+02:00 The Reflection of Low Frequency Sonar Signals from a Smooth Ocean Bottom. Part I. Experimental Reflection Losses at Locations off the California Coast and in the Bering Sea Whitney,J A Yee,G S Gardner,R R NAVY ELECTRONICS LAB SAN DIEGO CA 1963-01 text/html http://www.dtic.mil/docs/citations/ADA074407 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA074407 en eng http://www.dtic.mil/docs/citations/ADA074407 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Acoustic Detection and Detectors Acoustics *SONAR SIGNALS *BOTTOM LOSS UNDERWATER ACOUSTICS ACOUSTIC VELOCITY OCEAN BOTTOM TOPOGRAPHY LOW FREQUENCY OCEAN BOTTOM SOILS NORTH PACIFIC OCEAN ACOUSTIC REFLECTION SEA TESTING BERING SEA MOST Project-2 Text 1963 ftdtic 2016-02-20T16:54:16Z Underwater acoustic tests in three different areas are discussed: Area I is in 200-fathom water while Areas II and III are deep-water, 2000-fathom areas. From the data obtained bottom reflection losses were computed as a function of grazing angle for low frequency, 0.7 to 3.0 kc sound pulses. Measurements in Area I utilized short pulses and acoustic-path geometries that would resolve the bottom reflected paths; the analysis was then accomplished by comparing the direct signal with the signal which suffers one bottom reflection. The experiments in the deep-water areas did not attempt acoustic path resolution and the bottom loss was derived from the difference between the measured propagation loss and the theoretical propagation loss for that range and for total reflection at the grazing angle. See also Part 2, AD-A074 408. Text Bering Sea Defense Technical Information Center: DTIC Technical Reports database Bering Sea Pacific
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Acoustic Detection and Detectors
Acoustics
*SONAR SIGNALS
*BOTTOM LOSS
UNDERWATER ACOUSTICS
ACOUSTIC VELOCITY
OCEAN BOTTOM TOPOGRAPHY
LOW FREQUENCY
OCEAN BOTTOM SOILS
NORTH PACIFIC OCEAN
ACOUSTIC REFLECTION
SEA TESTING
BERING SEA
MOST Project-2
spellingShingle Acoustic Detection and Detectors
Acoustics
*SONAR SIGNALS
*BOTTOM LOSS
UNDERWATER ACOUSTICS
ACOUSTIC VELOCITY
OCEAN BOTTOM TOPOGRAPHY
LOW FREQUENCY
OCEAN BOTTOM SOILS
NORTH PACIFIC OCEAN
ACOUSTIC REFLECTION
SEA TESTING
BERING SEA
MOST Project-2
Whitney,J A
Yee,G S
Gardner,R R
The Reflection of Low Frequency Sonar Signals from a Smooth Ocean Bottom. Part I. Experimental Reflection Losses at Locations off the California Coast and in the Bering Sea
topic_facet Acoustic Detection and Detectors
Acoustics
*SONAR SIGNALS
*BOTTOM LOSS
UNDERWATER ACOUSTICS
ACOUSTIC VELOCITY
OCEAN BOTTOM TOPOGRAPHY
LOW FREQUENCY
OCEAN BOTTOM SOILS
NORTH PACIFIC OCEAN
ACOUSTIC REFLECTION
SEA TESTING
BERING SEA
MOST Project-2
description Underwater acoustic tests in three different areas are discussed: Area I is in 200-fathom water while Areas II and III are deep-water, 2000-fathom areas. From the data obtained bottom reflection losses were computed as a function of grazing angle for low frequency, 0.7 to 3.0 kc sound pulses. Measurements in Area I utilized short pulses and acoustic-path geometries that would resolve the bottom reflected paths; the analysis was then accomplished by comparing the direct signal with the signal which suffers one bottom reflection. The experiments in the deep-water areas did not attempt acoustic path resolution and the bottom loss was derived from the difference between the measured propagation loss and the theoretical propagation loss for that range and for total reflection at the grazing angle. See also Part 2, AD-A074 408.
author2 NAVY ELECTRONICS LAB SAN DIEGO CA
format Text
author Whitney,J A
Yee,G S
Gardner,R R
author_facet Whitney,J A
Yee,G S
Gardner,R R
author_sort Whitney,J A
title The Reflection of Low Frequency Sonar Signals from a Smooth Ocean Bottom. Part I. Experimental Reflection Losses at Locations off the California Coast and in the Bering Sea
title_short The Reflection of Low Frequency Sonar Signals from a Smooth Ocean Bottom. Part I. Experimental Reflection Losses at Locations off the California Coast and in the Bering Sea
title_full The Reflection of Low Frequency Sonar Signals from a Smooth Ocean Bottom. Part I. Experimental Reflection Losses at Locations off the California Coast and in the Bering Sea
title_fullStr The Reflection of Low Frequency Sonar Signals from a Smooth Ocean Bottom. Part I. Experimental Reflection Losses at Locations off the California Coast and in the Bering Sea
title_full_unstemmed The Reflection of Low Frequency Sonar Signals from a Smooth Ocean Bottom. Part I. Experimental Reflection Losses at Locations off the California Coast and in the Bering Sea
title_sort reflection of low frequency sonar signals from a smooth ocean bottom. part i. experimental reflection losses at locations off the california coast and in the bering sea
publishDate 1963
url http://www.dtic.mil/docs/citations/ADA074407
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA074407
geographic Bering Sea
Pacific
geographic_facet Bering Sea
Pacific
genre Bering Sea
genre_facet Bering Sea
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA074407
op_rights APPROVED FOR PUBLIC RELEASE
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