Magnetospheric line radiation observations at Halley, Antarctica

Magnetospheric line Radiation (MLR) events are relatively narrowband VLF signals that sometimes drift in frequency, and have been observed in both ground based and satellite data sets. Line radiation has been attributed by some authors to be power line harmonic radiation (PLHR), generated from harmo...

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Published in:Journal of Geophysical Research: Space Physics
Main Authors: Rodger, Craig J., Clilverd, Mark A., Yearby, Keith H., Smith, Andy J.
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 1999
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/503781/
https://doi.org/10.1029/1999JA900153
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spelling ftnerc:oai:nora.nerc.ac.uk:503781 2023-05-15T13:48:08+02:00 Magnetospheric line radiation observations at Halley, Antarctica Rodger, Craig J. Clilverd, Mark A. Yearby, Keith H. Smith, Andy J. 1999 http://nora.nerc.ac.uk/id/eprint/503781/ https://doi.org/10.1029/1999JA900153 unknown American Geophysical Union Rodger, Craig J.; Clilverd, Mark A. orcid:0000-0002-7388-1529 Yearby, Keith H.; Smith, Andy J. 1999 Magnetospheric line radiation observations at Halley, Antarctica. Journal of Geophysical Research, 104 (A8). 17441-17447. https://doi.org/10.1029/1999JA900153 <https://doi.org/10.1029/1999JA900153> Publication - Article PeerReviewed 1999 ftnerc https://doi.org/10.1029/1999JA900153 2023-02-04T19:38:02Z Magnetospheric line Radiation (MLR) events are relatively narrowband VLF signals that sometimes drift in frequency, and have been observed in both ground based and satellite data sets. Line radiation has been attributed by some authors to be power line harmonic radiation (PLHR), generated from harmonics of the power transmission frequency (50 or 60 Hz) and radiated into the ionosphere and magnetosphere by long power lines. We present the result of a survey undertaken on the basis of measurements made of MLR events observed at Halley station, Antarctica (75°30′S, 26°54′W, L ≈ 4.3) in part of June 1995. Particular attention is given to the frequency spacing, drift rates, and amplitude of the MLR lines. MLR is present in 7.0% of the minute-long VLF recordings made at Halley. The MLR lines rise in frequency as often as they fall. However, these lines do not necessarily rise or fall monotonically and can oscillate while drifting. The Halley MLR has a wide range of line spacings and does not preferentially show spacings near harmonics of electrical transmission frequencies, either 50 Hz or 60 Hz. There is no correlation between the frequency drifts of the local 50 Hz Halley electrical supply and those of the observed MLR lines. The distribution of MLR line spacings observed in the Halley data has a roughly exponential form, suggesting a different mechanism for MLR than for PLHR. Article in Journal/Newspaper Antarc* Antarctica Antarctica Journal Natural Environment Research Council: NERC Open Research Archive Halley Station ENVELOPE(-26.541,-26.541,-75.581,-75.581) Journal of Geophysical Research: Space Physics 104 A8 17441 17447
institution Open Polar
collection Natural Environment Research Council: NERC Open Research Archive
op_collection_id ftnerc
language unknown
description Magnetospheric line Radiation (MLR) events are relatively narrowband VLF signals that sometimes drift in frequency, and have been observed in both ground based and satellite data sets. Line radiation has been attributed by some authors to be power line harmonic radiation (PLHR), generated from harmonics of the power transmission frequency (50 or 60 Hz) and radiated into the ionosphere and magnetosphere by long power lines. We present the result of a survey undertaken on the basis of measurements made of MLR events observed at Halley station, Antarctica (75°30′S, 26°54′W, L ≈ 4.3) in part of June 1995. Particular attention is given to the frequency spacing, drift rates, and amplitude of the MLR lines. MLR is present in 7.0% of the minute-long VLF recordings made at Halley. The MLR lines rise in frequency as often as they fall. However, these lines do not necessarily rise or fall monotonically and can oscillate while drifting. The Halley MLR has a wide range of line spacings and does not preferentially show spacings near harmonics of electrical transmission frequencies, either 50 Hz or 60 Hz. There is no correlation between the frequency drifts of the local 50 Hz Halley electrical supply and those of the observed MLR lines. The distribution of MLR line spacings observed in the Halley data has a roughly exponential form, suggesting a different mechanism for MLR than for PLHR.
format Article in Journal/Newspaper
author Rodger, Craig J.
Clilverd, Mark A.
Yearby, Keith H.
Smith, Andy J.
spellingShingle Rodger, Craig J.
Clilverd, Mark A.
Yearby, Keith H.
Smith, Andy J.
Magnetospheric line radiation observations at Halley, Antarctica
author_facet Rodger, Craig J.
Clilverd, Mark A.
Yearby, Keith H.
Smith, Andy J.
author_sort Rodger, Craig J.
title Magnetospheric line radiation observations at Halley, Antarctica
title_short Magnetospheric line radiation observations at Halley, Antarctica
title_full Magnetospheric line radiation observations at Halley, Antarctica
title_fullStr Magnetospheric line radiation observations at Halley, Antarctica
title_full_unstemmed Magnetospheric line radiation observations at Halley, Antarctica
title_sort magnetospheric line radiation observations at halley, antarctica
publisher American Geophysical Union
publishDate 1999
url http://nora.nerc.ac.uk/id/eprint/503781/
https://doi.org/10.1029/1999JA900153
long_lat ENVELOPE(-26.541,-26.541,-75.581,-75.581)
geographic Halley Station
geographic_facet Halley Station
genre Antarc*
Antarctica
Antarctica Journal
genre_facet Antarc*
Antarctica
Antarctica Journal
op_relation Rodger, Craig J.; Clilverd, Mark A. orcid:0000-0002-7388-1529
Yearby, Keith H.; Smith, Andy J. 1999 Magnetospheric line radiation observations at Halley, Antarctica. Journal of Geophysical Research, 104 (A8). 17441-17447. https://doi.org/10.1029/1999JA900153 <https://doi.org/10.1029/1999JA900153>
op_doi https://doi.org/10.1029/1999JA900153
container_title Journal of Geophysical Research: Space Physics
container_volume 104
container_issue A8
container_start_page 17441
op_container_end_page 17447
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