Digital Spectra of Artificially Stimulated VLF Emissions.

New features of artificially stimulated VLF emissions from the magnetosphere have been discovered by using high resolution digital spectral analysis techniques. Several hundred emissions triggered by three VLF transmitters (NAA, Omega, Siple Station, Antarctica) have been examined. The stimulated em...

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Bibliographic Details
Main Author: Stiles,Gardiner Stuart
Other Authors: STANFORD UNIV CALIF STANFORD ELECTRONICS LABS
Format: Text
Language:English
Published: 1974
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA022833
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA022833
id ftdtic:ADA022833
record_format openpolar
spelling ftdtic:ADA022833 2023-05-15T14:01:32+02:00 Digital Spectra of Artificially Stimulated VLF Emissions. Stiles,Gardiner Stuart STANFORD UNIV CALIF STANFORD ELECTRONICS LABS 1974-12 text/html http://www.dtic.mil/docs/citations/ADA022833 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA022833 en eng http://www.dtic.mil/docs/citations/ADA022833 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Atmospheric Physics Radiofrequency Wave Propagation *EMISSION *MAGNETOSPHERE *WHISTLERS DIGITAL SYSTEMS GROWTH(GENERAL) POWER SPECTRA ELECTRONS RESONANCE TRANSMITTERS TRAVELING WAVE TUBES VERY LOW FREQUENCY Text 1974 ftdtic 2016-02-20T10:45:18Z New features of artificially stimulated VLF emissions from the magnetosphere have been discovered by using high resolution digital spectral analysis techniques. Several hundred emissions triggered by three VLF transmitters (NAA, Omega, Siple Station, Antarctica) have been examined. The stimulated emissions initially grow at the frequency of the triggering signal. The emissions always initially rise above the frequency of the triggering signal; this rise is independent of the final slope of the emissions. The emissions characteristically show exponential growth in time with rates that vary from 25 to 250 dB/s. Growth may continue past termination of the triggering signal and appears to be independent of the emission frequency over a range of at least several hundred Hz. The growth also may cease prior to termination. Emission amplitudes may reach 30 dB or more above the level of the triggering signal. Studies of a limited set of the data indicate that lower growth rates are observed when emission activity is just beginning or just ending. These periods are usually characterized by falling rather than rising emissions. These observations are in good agreement with a theory that attributes the emissions to an interaction between the triggering signal and counter-streaming gyroresonant electrons. Text Antarc* Antarctica Defense Technical Information Center: DTIC Technical Reports database Siple ENVELOPE(-83.917,-83.917,-75.917,-75.917)
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Atmospheric Physics
Radiofrequency Wave Propagation
*EMISSION
*MAGNETOSPHERE
*WHISTLERS
DIGITAL SYSTEMS
GROWTH(GENERAL)
POWER SPECTRA
ELECTRONS
RESONANCE
TRANSMITTERS
TRAVELING WAVE TUBES
VERY LOW FREQUENCY
spellingShingle Atmospheric Physics
Radiofrequency Wave Propagation
*EMISSION
*MAGNETOSPHERE
*WHISTLERS
DIGITAL SYSTEMS
GROWTH(GENERAL)
POWER SPECTRA
ELECTRONS
RESONANCE
TRANSMITTERS
TRAVELING WAVE TUBES
VERY LOW FREQUENCY
Stiles,Gardiner Stuart
Digital Spectra of Artificially Stimulated VLF Emissions.
topic_facet Atmospheric Physics
Radiofrequency Wave Propagation
*EMISSION
*MAGNETOSPHERE
*WHISTLERS
DIGITAL SYSTEMS
GROWTH(GENERAL)
POWER SPECTRA
ELECTRONS
RESONANCE
TRANSMITTERS
TRAVELING WAVE TUBES
VERY LOW FREQUENCY
description New features of artificially stimulated VLF emissions from the magnetosphere have been discovered by using high resolution digital spectral analysis techniques. Several hundred emissions triggered by three VLF transmitters (NAA, Omega, Siple Station, Antarctica) have been examined. The stimulated emissions initially grow at the frequency of the triggering signal. The emissions always initially rise above the frequency of the triggering signal; this rise is independent of the final slope of the emissions. The emissions characteristically show exponential growth in time with rates that vary from 25 to 250 dB/s. Growth may continue past termination of the triggering signal and appears to be independent of the emission frequency over a range of at least several hundred Hz. The growth also may cease prior to termination. Emission amplitudes may reach 30 dB or more above the level of the triggering signal. Studies of a limited set of the data indicate that lower growth rates are observed when emission activity is just beginning or just ending. These periods are usually characterized by falling rather than rising emissions. These observations are in good agreement with a theory that attributes the emissions to an interaction between the triggering signal and counter-streaming gyroresonant electrons.
author2 STANFORD UNIV CALIF STANFORD ELECTRONICS LABS
format Text
author Stiles,Gardiner Stuart
author_facet Stiles,Gardiner Stuart
author_sort Stiles,Gardiner Stuart
title Digital Spectra of Artificially Stimulated VLF Emissions.
title_short Digital Spectra of Artificially Stimulated VLF Emissions.
title_full Digital Spectra of Artificially Stimulated VLF Emissions.
title_fullStr Digital Spectra of Artificially Stimulated VLF Emissions.
title_full_unstemmed Digital Spectra of Artificially Stimulated VLF Emissions.
title_sort digital spectra of artificially stimulated vlf emissions.
publishDate 1974
url http://www.dtic.mil/docs/citations/ADA022833
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA022833
long_lat ENVELOPE(-83.917,-83.917,-75.917,-75.917)
geographic Siple
geographic_facet Siple
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA022833
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766271379309592576