TRANSAURORAL HIGH FREQUENCY RADIO PROPAGATION. VOLUME I. SIGNAL AMPLITUDE OBSERVATIONS.
Pulsed signals of 11 and 17 mc were transmitted over the transauroral path from Thule, Greenland to Norwood, Massachusetts. This path, which is perpendicular to the auororal zone, has its midpoint near Fort Chimo, Canada in the region of maximum auroral activity. At the Norwood receiving terminal, c...
Main Author: | |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Published: |
1965
|
Subjects: | |
Online Access: | http://www.dtic.mil/docs/citations/AD0620683 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0620683 |
id |
ftdtic:AD0620683 |
---|---|
record_format |
openpolar |
spelling |
ftdtic:AD0620683 2023-05-15T15:02:38+02:00 TRANSAURORAL HIGH FREQUENCY RADIO PROPAGATION. VOLUME I. SIGNAL AMPLITUDE OBSERVATIONS. Roberts,Frank R. RAYTHEON CO NORWOOD MASS 1965-04 text/html http://www.dtic.mil/docs/citations/AD0620683 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0620683 en eng http://www.dtic.mil/docs/citations/AD0620683 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS ATMOSPHERICS AURORAE ARCTIC REGIONS RADIOFREQUENCY PULSES GREENLAND MASSACHUSETTS RADIO WAVES ELECTROMAGNETIC RADIATION GEOPHYSICS Text 1965 ftdtic 2016-02-21T22:39:57Z Pulsed signals of 11 and 17 mc were transmitted over the transauroral path from Thule, Greenland to Norwood, Massachusetts. This path, which is perpendicular to the auororal zone, has its midpoint near Fort Chimo, Canada in the region of maximum auroral activity. At the Norwood receiving terminal, continuous recording of signal amplitude was performed over a 17-month period. Graphical presentations of circuit performance illustrate diurnal and seasonal variations, together with the dependence on geomagetic activity. Normal propagation is F-layer controlled, although it departs markedly from classical predictions. Results of a theoretical investigation indicate that ionspheric layer tilts play no significant role in these departures. The occasional occurrence of anomalous modes is evident in the data. Absorption events coincident with reported shortwave fadeouts are noted. (Author) Text Arctic Greenland Thule Defense Technical Information Center: DTIC Technical Reports database Arctic Canada Greenland |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
ATMOSPHERICS AURORAE ARCTIC REGIONS RADIOFREQUENCY PULSES GREENLAND MASSACHUSETTS RADIO WAVES ELECTROMAGNETIC RADIATION GEOPHYSICS |
spellingShingle |
ATMOSPHERICS AURORAE ARCTIC REGIONS RADIOFREQUENCY PULSES GREENLAND MASSACHUSETTS RADIO WAVES ELECTROMAGNETIC RADIATION GEOPHYSICS Roberts,Frank R. TRANSAURORAL HIGH FREQUENCY RADIO PROPAGATION. VOLUME I. SIGNAL AMPLITUDE OBSERVATIONS. |
topic_facet |
ATMOSPHERICS AURORAE ARCTIC REGIONS RADIOFREQUENCY PULSES GREENLAND MASSACHUSETTS RADIO WAVES ELECTROMAGNETIC RADIATION GEOPHYSICS |
description |
Pulsed signals of 11 and 17 mc were transmitted over the transauroral path from Thule, Greenland to Norwood, Massachusetts. This path, which is perpendicular to the auororal zone, has its midpoint near Fort Chimo, Canada in the region of maximum auroral activity. At the Norwood receiving terminal, continuous recording of signal amplitude was performed over a 17-month period. Graphical presentations of circuit performance illustrate diurnal and seasonal variations, together with the dependence on geomagetic activity. Normal propagation is F-layer controlled, although it departs markedly from classical predictions. Results of a theoretical investigation indicate that ionspheric layer tilts play no significant role in these departures. The occasional occurrence of anomalous modes is evident in the data. Absorption events coincident with reported shortwave fadeouts are noted. (Author) |
author2 |
RAYTHEON CO NORWOOD MASS |
format |
Text |
author |
Roberts,Frank R. |
author_facet |
Roberts,Frank R. |
author_sort |
Roberts,Frank R. |
title |
TRANSAURORAL HIGH FREQUENCY RADIO PROPAGATION. VOLUME I. SIGNAL AMPLITUDE OBSERVATIONS. |
title_short |
TRANSAURORAL HIGH FREQUENCY RADIO PROPAGATION. VOLUME I. SIGNAL AMPLITUDE OBSERVATIONS. |
title_full |
TRANSAURORAL HIGH FREQUENCY RADIO PROPAGATION. VOLUME I. SIGNAL AMPLITUDE OBSERVATIONS. |
title_fullStr |
TRANSAURORAL HIGH FREQUENCY RADIO PROPAGATION. VOLUME I. SIGNAL AMPLITUDE OBSERVATIONS. |
title_full_unstemmed |
TRANSAURORAL HIGH FREQUENCY RADIO PROPAGATION. VOLUME I. SIGNAL AMPLITUDE OBSERVATIONS. |
title_sort |
transauroral high frequency radio propagation. volume i. signal amplitude observations. |
publishDate |
1965 |
url |
http://www.dtic.mil/docs/citations/AD0620683 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0620683 |
geographic |
Arctic Canada Greenland |
geographic_facet |
Arctic Canada Greenland |
genre |
Arctic Greenland Thule |
genre_facet |
Arctic Greenland Thule |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0620683 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766334568309194752 |