Fresnel Zone Theory of VLF Coupling into the Earth-Ionosphere Waveguide.

VLF propagation over long paths does not fill the entire great circle arc between transmitter and receiver at the ionospheric altitude. It is blind to the appearance of the terminator over either station. This report concerns one method of calculating the spacial extent of these 'excitation...

Full description

Bibliographic Details
Main Author: Bradford, W. R.
Other Authors: NAVAL ELECTRONICS LAB CENTER SAN DIEGO CA
Format: Text
Language:English
Published: 1971
Subjects:
Online Access:http://www.dtic.mil/docs/citations/AD0892152
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0892152
id ftdtic:AD0892152
record_format openpolar
spelling ftdtic:AD0892152 2023-05-15T16:29:14+02:00 Fresnel Zone Theory of VLF Coupling into the Earth-Ionosphere Waveguide. Bradford, W. R. NAVAL ELECTRONICS LAB CENTER SAN DIEGO CA 1971-07-22 text/html http://www.dtic.mil/docs/citations/AD0892152 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0892152 en eng http://www.dtic.mil/docs/citations/AD0892152 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Cybernetics Radiofrequency Wave Propagation Radio Communications (*RADIO TRANSMISSION THEORY) (*RADIO RECEPTION VERY LOW FREQUENCY) (*INFORMATION THEORY PROPAGATION) RADIO TRANSMITTERS RADIO RECEIVERS WAVEGUIDES IONOSPHERE EARTH(PLANET) DIURNAL VARIATIONS INTERFACES REFLECTIVITY GREENLAND NORWAY EIGENANGLES FRESNEL ZONES RAY TRACING Text 1971 ftdtic 2016-02-19T07:11:24Z VLF propagation over long paths does not fill the entire great circle arc between transmitter and receiver at the ionospheric altitude. It is blind to the appearance of the terminator over either station. This report concerns one method of calculating the spacial extent of these 'excitation' regions. A ray is drawn from the transmitting station so its angle of incidence at the ionosphere is the real part of the eigenangle. Other rays in the plane of incidence intersect the ionosphere in a great circle arc. The Fresnel zone phase coherence criterion, + or - one quarterwave, is applied to limit the extent of this arc. The arithmetic mean of central angles from the transmitter to each end of the arc is a measure of the excitation region. Calculations are carried out for 12 eigenangles. These represent day and night profiles at three latitudes over water. The Thule-Norway path is also represented. Text Greenland Thule Defense Technical Information Center: DTIC Technical Reports database Greenland Norway
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Cybernetics
Radiofrequency Wave Propagation
Radio Communications
(*RADIO TRANSMISSION
THEORY)
(*RADIO RECEPTION
VERY LOW FREQUENCY)
(*INFORMATION THEORY
PROPAGATION)
RADIO TRANSMITTERS
RADIO RECEIVERS
WAVEGUIDES
IONOSPHERE
EARTH(PLANET)
DIURNAL VARIATIONS
INTERFACES
REFLECTIVITY
GREENLAND
NORWAY
EIGENANGLES
FRESNEL ZONES
RAY TRACING
spellingShingle Cybernetics
Radiofrequency Wave Propagation
Radio Communications
(*RADIO TRANSMISSION
THEORY)
(*RADIO RECEPTION
VERY LOW FREQUENCY)
(*INFORMATION THEORY
PROPAGATION)
RADIO TRANSMITTERS
RADIO RECEIVERS
WAVEGUIDES
IONOSPHERE
EARTH(PLANET)
DIURNAL VARIATIONS
INTERFACES
REFLECTIVITY
GREENLAND
NORWAY
EIGENANGLES
FRESNEL ZONES
RAY TRACING
Bradford, W. R.
Fresnel Zone Theory of VLF Coupling into the Earth-Ionosphere Waveguide.
topic_facet Cybernetics
Radiofrequency Wave Propagation
Radio Communications
(*RADIO TRANSMISSION
THEORY)
(*RADIO RECEPTION
VERY LOW FREQUENCY)
(*INFORMATION THEORY
PROPAGATION)
RADIO TRANSMITTERS
RADIO RECEIVERS
WAVEGUIDES
IONOSPHERE
EARTH(PLANET)
DIURNAL VARIATIONS
INTERFACES
REFLECTIVITY
GREENLAND
NORWAY
EIGENANGLES
FRESNEL ZONES
RAY TRACING
description VLF propagation over long paths does not fill the entire great circle arc between transmitter and receiver at the ionospheric altitude. It is blind to the appearance of the terminator over either station. This report concerns one method of calculating the spacial extent of these 'excitation' regions. A ray is drawn from the transmitting station so its angle of incidence at the ionosphere is the real part of the eigenangle. Other rays in the plane of incidence intersect the ionosphere in a great circle arc. The Fresnel zone phase coherence criterion, + or - one quarterwave, is applied to limit the extent of this arc. The arithmetic mean of central angles from the transmitter to each end of the arc is a measure of the excitation region. Calculations are carried out for 12 eigenangles. These represent day and night profiles at three latitudes over water. The Thule-Norway path is also represented.
author2 NAVAL ELECTRONICS LAB CENTER SAN DIEGO CA
format Text
author Bradford, W. R.
author_facet Bradford, W. R.
author_sort Bradford, W. R.
title Fresnel Zone Theory of VLF Coupling into the Earth-Ionosphere Waveguide.
title_short Fresnel Zone Theory of VLF Coupling into the Earth-Ionosphere Waveguide.
title_full Fresnel Zone Theory of VLF Coupling into the Earth-Ionosphere Waveguide.
title_fullStr Fresnel Zone Theory of VLF Coupling into the Earth-Ionosphere Waveguide.
title_full_unstemmed Fresnel Zone Theory of VLF Coupling into the Earth-Ionosphere Waveguide.
title_sort fresnel zone theory of vlf coupling into the earth-ionosphere waveguide.
publishDate 1971
url http://www.dtic.mil/docs/citations/AD0892152
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0892152
geographic Greenland
Norway
geographic_facet Greenland
Norway
genre Greenland
Thule
genre_facet Greenland
Thule
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0892152
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766018924022857728