Multipath Propagation over Snow at Millimeter Wavelengths
A series of multipath measurements over snow were conducted at Hanscom AFB during the winter 1978/1979. Data were obtained over a path-length of 179.5 m at frequencies of 35, 98, and 140 GHz. The gently rolling grass-covered terrain showed maximum height differences of 0.8 m. Snow covers included fr...
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ftdtic:ADA087747 2023-05-15T16:37:52+02:00 Multipath Propagation over Snow at Millimeter Wavelengths Lammers,Uve H W Hayes,Dallas T ROME AIR DEVELOPMENT CENTER GRIFFISS AFB NY 1980-02 text/html http://www.dtic.mil/docs/citations/ADA087747 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA087747 en eng http://www.dtic.mil/docs/citations/ADA087747 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Computer Programming and Software Radiofrequency Wave Propagation *SNOW COVER *MULTIPATH TRANSMISSION *RADIATION PATTERNS *INTERFERENCE ANALYZERS COMPUTER PROGRAMS CONTINUOUS WAVES MILLIMETER WAVES RECEIVERS TRANSMITTERS EXTREMELY HIGH FREQUENCY KA BAND LOW ANGLES SPECULAR REFLECTION GRAZING Height gain patterns Metamorphic snow Terrain reflected rays Grass covered terrain Terrain height M Band Grazing angles PE62702F WURADC46001607 Text 1980 ftdtic 2016-02-20T18:26:15Z A series of multipath measurements over snow were conducted at Hanscom AFB during the winter 1978/1979. Data were obtained over a path-length of 179.5 m at frequencies of 35, 98, and 140 GHz. The gently rolling grass-covered terrain showed maximum height differences of 0.8 m. Snow covers included freshly fallen snow, old metamorphic snow, and sleet. The equipment consisted of CW transmitters at 2-m height and receivers mounted on a vertical positioner to measure the height-gain pattern of the received signal between 0.2- and 4-m height. Grazing angles for this geometry range between 0.5 and 2 degrees. Measured interference patterns between direct and terrain-reflected rays were generally coherent in appearance and exhibited cancellation depths of 20 dB and lower, depending on the type of snow cover. A computer program was developed in order to model the reflection as a specular process, with the underlying terrain represented by a series of linear sloping segments, derived from actual terrain height measurements. With appropriate transitions between the linear segments and reflection coefficients calculated from relevant snow parameters, calculated and measured height-gain patterns display quite similar qualities. (Author) Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Snow Ice and Permafrost Computer Programming and Software Radiofrequency Wave Propagation *SNOW COVER *MULTIPATH TRANSMISSION *RADIATION PATTERNS *INTERFERENCE ANALYZERS COMPUTER PROGRAMS CONTINUOUS WAVES MILLIMETER WAVES RECEIVERS TRANSMITTERS EXTREMELY HIGH FREQUENCY KA BAND LOW ANGLES SPECULAR REFLECTION GRAZING Height gain patterns Metamorphic snow Terrain reflected rays Grass covered terrain Terrain height M Band Grazing angles PE62702F WURADC46001607 |
spellingShingle |
Snow Ice and Permafrost Computer Programming and Software Radiofrequency Wave Propagation *SNOW COVER *MULTIPATH TRANSMISSION *RADIATION PATTERNS *INTERFERENCE ANALYZERS COMPUTER PROGRAMS CONTINUOUS WAVES MILLIMETER WAVES RECEIVERS TRANSMITTERS EXTREMELY HIGH FREQUENCY KA BAND LOW ANGLES SPECULAR REFLECTION GRAZING Height gain patterns Metamorphic snow Terrain reflected rays Grass covered terrain Terrain height M Band Grazing angles PE62702F WURADC46001607 Lammers,Uve H W Hayes,Dallas T Multipath Propagation over Snow at Millimeter Wavelengths |
topic_facet |
Snow Ice and Permafrost Computer Programming and Software Radiofrequency Wave Propagation *SNOW COVER *MULTIPATH TRANSMISSION *RADIATION PATTERNS *INTERFERENCE ANALYZERS COMPUTER PROGRAMS CONTINUOUS WAVES MILLIMETER WAVES RECEIVERS TRANSMITTERS EXTREMELY HIGH FREQUENCY KA BAND LOW ANGLES SPECULAR REFLECTION GRAZING Height gain patterns Metamorphic snow Terrain reflected rays Grass covered terrain Terrain height M Band Grazing angles PE62702F WURADC46001607 |
description |
A series of multipath measurements over snow were conducted at Hanscom AFB during the winter 1978/1979. Data were obtained over a path-length of 179.5 m at frequencies of 35, 98, and 140 GHz. The gently rolling grass-covered terrain showed maximum height differences of 0.8 m. Snow covers included freshly fallen snow, old metamorphic snow, and sleet. The equipment consisted of CW transmitters at 2-m height and receivers mounted on a vertical positioner to measure the height-gain pattern of the received signal between 0.2- and 4-m height. Grazing angles for this geometry range between 0.5 and 2 degrees. Measured interference patterns between direct and terrain-reflected rays were generally coherent in appearance and exhibited cancellation depths of 20 dB and lower, depending on the type of snow cover. A computer program was developed in order to model the reflection as a specular process, with the underlying terrain represented by a series of linear sloping segments, derived from actual terrain height measurements. With appropriate transitions between the linear segments and reflection coefficients calculated from relevant snow parameters, calculated and measured height-gain patterns display quite similar qualities. (Author) |
author2 |
ROME AIR DEVELOPMENT CENTER GRIFFISS AFB NY |
format |
Text |
author |
Lammers,Uve H W Hayes,Dallas T |
author_facet |
Lammers,Uve H W Hayes,Dallas T |
author_sort |
Lammers,Uve H W |
title |
Multipath Propagation over Snow at Millimeter Wavelengths |
title_short |
Multipath Propagation over Snow at Millimeter Wavelengths |
title_full |
Multipath Propagation over Snow at Millimeter Wavelengths |
title_fullStr |
Multipath Propagation over Snow at Millimeter Wavelengths |
title_full_unstemmed |
Multipath Propagation over Snow at Millimeter Wavelengths |
title_sort |
multipath propagation over snow at millimeter wavelengths |
publishDate |
1980 |
url |
http://www.dtic.mil/docs/citations/ADA087747 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA087747 |
genre |
Ice permafrost |
genre_facet |
Ice permafrost |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA087747 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766028157488463872 |