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...
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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 |