METEOROLOGICAL CONDITIONS AFFECTING ARCTIC SOUND PROPAGATION

A description of the effects of vertical temperature distribution and wind on the propagation of sound in the lowest layers of the Arctic atmosphere. Variations in temperature profiles are examined seasonally, daily, and diurnally under various wind conditions, and the behavior of the wind within th...

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Bibliographic Details
Main Authors: Batten,E. S., Schutz,C.
Other Authors: RAND CORP SANTA MONICA CALIF
Format: Text
Language:English
Published: 1968
Subjects:
Online Access:http://www.dtic.mil/docs/citations/AD0679545
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0679545
id ftdtic:AD0679545
record_format openpolar
spelling ftdtic:AD0679545 2023-05-15T14:47:02+02:00 METEOROLOGICAL CONDITIONS AFFECTING ARCTIC SOUND PROPAGATION Batten,E. S. Schutz,C. RAND CORP SANTA MONICA CALIF 1968-11 text/html http://www.dtic.mil/docs/citations/AD0679545 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0679545 en eng http://www.dtic.mil/docs/citations/AD0679545 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Meteorology Acoustics (*METEOROLOGICAL PHENOMENA *ARCTIC REGIONS) (*SOUND TRANSMISSION ATMOSPHERES) WIND ATMOSPHERIC TEMPERATURE DETECTION VELOCITY DISTRIBUTION AUDITORY PERCEPTION FRICTION TWILIGHT THERMAL STABILITY PERIODIC VARIATIONS STATISTICAL ANALYSIS DIURNAL VARIATIONS POLAR REGIONS LAYERS(ATMOSPHERE) SUMMER WINTER Text 1968 ftdtic 2016-02-18T21:33:02Z A description of the effects of vertical temperature distribution and wind on the propagation of sound in the lowest layers of the Arctic atmosphere. Variations in temperature profiles are examined seasonally, daily, and diurnally under various wind conditions, and the behavior of the wind within the friction layer of the atmosphere is explored. The theory of the Ekman spiral is used to compute the theoretical distribution of wind speed and sound speed as a function of azimuth for three characteristic temperature profiles as a function of azimuth. Considering temperature alone, the calculations show that supernormal audibility will probably be common during the polar night and perhaps during the summer twilight. (Author) Text Arctic polar night Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Sound ENVELOPE(-108.852,-108.852,67.534,67.534)
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Meteorology
Acoustics
(*METEOROLOGICAL PHENOMENA
*ARCTIC REGIONS)
(*SOUND TRANSMISSION
ATMOSPHERES)
WIND
ATMOSPHERIC TEMPERATURE
DETECTION
VELOCITY
DISTRIBUTION
AUDITORY PERCEPTION
FRICTION
TWILIGHT
THERMAL STABILITY
PERIODIC VARIATIONS
STATISTICAL ANALYSIS
DIURNAL VARIATIONS
POLAR REGIONS
LAYERS(ATMOSPHERE)
SUMMER
WINTER
spellingShingle Meteorology
Acoustics
(*METEOROLOGICAL PHENOMENA
*ARCTIC REGIONS)
(*SOUND TRANSMISSION
ATMOSPHERES)
WIND
ATMOSPHERIC TEMPERATURE
DETECTION
VELOCITY
DISTRIBUTION
AUDITORY PERCEPTION
FRICTION
TWILIGHT
THERMAL STABILITY
PERIODIC VARIATIONS
STATISTICAL ANALYSIS
DIURNAL VARIATIONS
POLAR REGIONS
LAYERS(ATMOSPHERE)
SUMMER
WINTER
Batten,E. S.
Schutz,C.
METEOROLOGICAL CONDITIONS AFFECTING ARCTIC SOUND PROPAGATION
topic_facet Meteorology
Acoustics
(*METEOROLOGICAL PHENOMENA
*ARCTIC REGIONS)
(*SOUND TRANSMISSION
ATMOSPHERES)
WIND
ATMOSPHERIC TEMPERATURE
DETECTION
VELOCITY
DISTRIBUTION
AUDITORY PERCEPTION
FRICTION
TWILIGHT
THERMAL STABILITY
PERIODIC VARIATIONS
STATISTICAL ANALYSIS
DIURNAL VARIATIONS
POLAR REGIONS
LAYERS(ATMOSPHERE)
SUMMER
WINTER
description A description of the effects of vertical temperature distribution and wind on the propagation of sound in the lowest layers of the Arctic atmosphere. Variations in temperature profiles are examined seasonally, daily, and diurnally under various wind conditions, and the behavior of the wind within the friction layer of the atmosphere is explored. The theory of the Ekman spiral is used to compute the theoretical distribution of wind speed and sound speed as a function of azimuth for three characteristic temperature profiles as a function of azimuth. Considering temperature alone, the calculations show that supernormal audibility will probably be common during the polar night and perhaps during the summer twilight. (Author)
author2 RAND CORP SANTA MONICA CALIF
format Text
author Batten,E. S.
Schutz,C.
author_facet Batten,E. S.
Schutz,C.
author_sort Batten,E. S.
title METEOROLOGICAL CONDITIONS AFFECTING ARCTIC SOUND PROPAGATION
title_short METEOROLOGICAL CONDITIONS AFFECTING ARCTIC SOUND PROPAGATION
title_full METEOROLOGICAL CONDITIONS AFFECTING ARCTIC SOUND PROPAGATION
title_fullStr METEOROLOGICAL CONDITIONS AFFECTING ARCTIC SOUND PROPAGATION
title_full_unstemmed METEOROLOGICAL CONDITIONS AFFECTING ARCTIC SOUND PROPAGATION
title_sort meteorological conditions affecting arctic sound propagation
publishDate 1968
url http://www.dtic.mil/docs/citations/AD0679545
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0679545
long_lat ENVELOPE(-108.852,-108.852,67.534,67.534)
geographic Arctic
Arctic Sound
geographic_facet Arctic
Arctic Sound
genre Arctic
polar night
genre_facet Arctic
polar night
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0679545
op_rights APPROVED FOR PUBLIC RELEASE
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