Arctic Atmospheric Noise and Propagation Studies. Part A. Arctic Sferic Data--August 1958 to March 1969

From August 1958 through March 1959 Stanford Research Institute operated sferic monitoring stations at Fairbanks, Alaska, at Thule, Greenland, and at St. Johns, Newfoundland to record sferic 3- to 30-kc waveforms, direction of arrival, and rates of occurrence of sferics, and atmospheric noise levels...

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Main Author: Whitson, A. L.
Other Authors: STANFORD RESEARCH INST MENLO PARK CA
Format: Text
Language:English
Published: 1960
Subjects:
Online Access:http://www.dtic.mil/docs/citations/AD0752247
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0752247
id ftdtic:AD0752247
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spelling ftdtic:AD0752247 2023-05-15T14:47:53+02:00 Arctic Atmospheric Noise and Propagation Studies. Part A. Arctic Sferic Data--August 1958 to March 1969 Whitson, A. L. STANFORD RESEARCH INST MENLO PARK CA 1960-02 text/html http://www.dtic.mil/docs/citations/AD0752247 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0752247 en eng http://www.dtic.mil/docs/citations/AD0752247 Approved for public release; distribution is unlimited. DTIC AND NTIS Atmospheric Physics *ATMOSPHERICS CORRELATION TECHNIQUES DIURNAL VARIATIONS ARCTIC REGIONS SOLAR DISTURBANCES VERY LOW FREQUENCY IONOSPHERIC PROPAGATION EXTREMELY LOW FREQUENCY ATMOSPHERICS Text 1960 ftdtic 2016-02-22T11:57:07Z From August 1958 through March 1959 Stanford Research Institute operated sferic monitoring stations at Fairbanks, Alaska, at Thule, Greenland, and at St. Johns, Newfoundland to record sferic 3- to 30-kc waveforms, direction of arrival, and rates of occurrence of sferics, and atmospheric noise levels from 12 to 30 kc. Large amounts of the above data have been recorded. Also, uniformly distributed samples of the data have been analyzed to determine sferic amplitude and direction-of-arrival distributions, sferic waveform types, sferic ELF content, sferic source locations in all portions of the Northern Hemisphere, and RMS atmospheric noise levels as functions of time of day and season. In addition, the application of the data collected to the better understanding of VLF propagation and of the influence of geophysical phenomena are discussed. Text Arctic Greenland Newfoundland Thule Alaska Defense Technical Information Center: DTIC Technical Reports database Arctic Fairbanks Greenland
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Atmospheric Physics
*ATMOSPHERICS
CORRELATION TECHNIQUES
DIURNAL VARIATIONS
ARCTIC REGIONS
SOLAR DISTURBANCES
VERY LOW FREQUENCY
IONOSPHERIC PROPAGATION
EXTREMELY LOW FREQUENCY
ATMOSPHERICS
spellingShingle Atmospheric Physics
*ATMOSPHERICS
CORRELATION TECHNIQUES
DIURNAL VARIATIONS
ARCTIC REGIONS
SOLAR DISTURBANCES
VERY LOW FREQUENCY
IONOSPHERIC PROPAGATION
EXTREMELY LOW FREQUENCY
ATMOSPHERICS
Whitson, A. L.
Arctic Atmospheric Noise and Propagation Studies. Part A. Arctic Sferic Data--August 1958 to March 1969
topic_facet Atmospheric Physics
*ATMOSPHERICS
CORRELATION TECHNIQUES
DIURNAL VARIATIONS
ARCTIC REGIONS
SOLAR DISTURBANCES
VERY LOW FREQUENCY
IONOSPHERIC PROPAGATION
EXTREMELY LOW FREQUENCY
ATMOSPHERICS
description From August 1958 through March 1959 Stanford Research Institute operated sferic monitoring stations at Fairbanks, Alaska, at Thule, Greenland, and at St. Johns, Newfoundland to record sferic 3- to 30-kc waveforms, direction of arrival, and rates of occurrence of sferics, and atmospheric noise levels from 12 to 30 kc. Large amounts of the above data have been recorded. Also, uniformly distributed samples of the data have been analyzed to determine sferic amplitude and direction-of-arrival distributions, sferic waveform types, sferic ELF content, sferic source locations in all portions of the Northern Hemisphere, and RMS atmospheric noise levels as functions of time of day and season. In addition, the application of the data collected to the better understanding of VLF propagation and of the influence of geophysical phenomena are discussed.
author2 STANFORD RESEARCH INST MENLO PARK CA
format Text
author Whitson, A. L.
author_facet Whitson, A. L.
author_sort Whitson, A. L.
title Arctic Atmospheric Noise and Propagation Studies. Part A. Arctic Sferic Data--August 1958 to March 1969
title_short Arctic Atmospheric Noise and Propagation Studies. Part A. Arctic Sferic Data--August 1958 to March 1969
title_full Arctic Atmospheric Noise and Propagation Studies. Part A. Arctic Sferic Data--August 1958 to March 1969
title_fullStr Arctic Atmospheric Noise and Propagation Studies. Part A. Arctic Sferic Data--August 1958 to March 1969
title_full_unstemmed Arctic Atmospheric Noise and Propagation Studies. Part A. Arctic Sferic Data--August 1958 to March 1969
title_sort arctic atmospheric noise and propagation studies. part a. arctic sferic data--august 1958 to march 1969
publishDate 1960
url http://www.dtic.mil/docs/citations/AD0752247
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0752247
geographic Arctic
Fairbanks
Greenland
geographic_facet Arctic
Fairbanks
Greenland
genre Arctic
Greenland
Newfoundland
Thule
Alaska
genre_facet Arctic
Greenland
Newfoundland
Thule
Alaska
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0752247
op_rights Approved for public release; distribution is unlimited.
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