Magnetospheric VLF line radiation.

Magnetospheric VLF Line Radiation (MLR) is a broad band VLF emission (typically 1 kHz wide centered on 3 kHz) which has line structure in its spectrum. The events studied were received during 1977-80 at Halley, Antarctica and also in the geomagnetically conjugate region (Newfoundland). The occurrenc...

Full description

Bibliographic Details
Main Author: Yearby, Keith Howard
Format: Thesis
Language:English
Published: University of Sheffield 1983
Subjects:
Online Access:https://etheses.whiterose.ac.uk/21743/
https://etheses.whiterose.ac.uk/21743/1/256707.pdf
id ftwhiterose:oai:etheses.whiterose.ac.uk:21743
record_format openpolar
spelling ftwhiterose:oai:etheses.whiterose.ac.uk:21743 2023-05-15T13:50:32+02:00 Magnetospheric VLF line radiation. Yearby, Keith Howard 1983 text https://etheses.whiterose.ac.uk/21743/ https://etheses.whiterose.ac.uk/21743/1/256707.pdf en eng University of Sheffield https://etheses.whiterose.ac.uk/21743/1/256707.pdf Yearby, Keith Howard (1983) Magnetospheric VLF line radiation. PhD thesis, University of Sheffield. Thesis NonPeerReviewed 1983 ftwhiterose 2023-01-30T21:25:43Z Magnetospheric VLF Line Radiation (MLR) is a broad band VLF emission (typically 1 kHz wide centered on 3 kHz) which has line structure in its spectrum. The events studied were received during 1977-80 at Halley, Antarctica and also in the geomagnetically conjugate region (Newfoundland). The occurrence of Halley MLR events as a function of local time and geomagnetic activity and the differences in MLR activity between Halley and SipLe, Antarctica are discussed. An MLR event received on 26 June 1978 may be the result of magnetospheric amplification of VLF radiation of harmonics from electrical power lines (PLHR) in the conjugate region; the radiated power required was estimated to be 50 mW. Most Halley MLR events do not have any direct relation with PLHR although in several of the generation mechanisms discussed PLHR may have an indirect role. A series of measurements of the electromagnetic field near to several power transmission Lines in Newfoundland were made to determine the magnitude of the unbalanced harmonic currents and the skin depth in the ground, which in turn were used to estimate the strength of PLHR entering the magnetosphere. The largest radiated power determined for a single line was 500 nW in the range 2.7 to 3.7 kHz although much Larger powers may be radiated from the more industrialised regions further west. A description of the VLF receiver and some improvements made to it is given followed by a review of spectrum analysis techniques and a description of some methods used for the work on PLHR and MLR. Thesis Antarc* Antarctica Newfoundland White Rose eTheses Online (Universities Leeds, Sheffield, York) Siple ENVELOPE(-83.917,-83.917,-75.917,-75.917)
institution Open Polar
collection White Rose eTheses Online (Universities Leeds, Sheffield, York)
op_collection_id ftwhiterose
language English
description Magnetospheric VLF Line Radiation (MLR) is a broad band VLF emission (typically 1 kHz wide centered on 3 kHz) which has line structure in its spectrum. The events studied were received during 1977-80 at Halley, Antarctica and also in the geomagnetically conjugate region (Newfoundland). The occurrence of Halley MLR events as a function of local time and geomagnetic activity and the differences in MLR activity between Halley and SipLe, Antarctica are discussed. An MLR event received on 26 June 1978 may be the result of magnetospheric amplification of VLF radiation of harmonics from electrical power lines (PLHR) in the conjugate region; the radiated power required was estimated to be 50 mW. Most Halley MLR events do not have any direct relation with PLHR although in several of the generation mechanisms discussed PLHR may have an indirect role. A series of measurements of the electromagnetic field near to several power transmission Lines in Newfoundland were made to determine the magnitude of the unbalanced harmonic currents and the skin depth in the ground, which in turn were used to estimate the strength of PLHR entering the magnetosphere. The largest radiated power determined for a single line was 500 nW in the range 2.7 to 3.7 kHz although much Larger powers may be radiated from the more industrialised regions further west. A description of the VLF receiver and some improvements made to it is given followed by a review of spectrum analysis techniques and a description of some methods used for the work on PLHR and MLR.
format Thesis
author Yearby, Keith Howard
spellingShingle Yearby, Keith Howard
Magnetospheric VLF line radiation.
author_facet Yearby, Keith Howard
author_sort Yearby, Keith Howard
title Magnetospheric VLF line radiation.
title_short Magnetospheric VLF line radiation.
title_full Magnetospheric VLF line radiation.
title_fullStr Magnetospheric VLF line radiation.
title_full_unstemmed Magnetospheric VLF line radiation.
title_sort magnetospheric vlf line radiation.
publisher University of Sheffield
publishDate 1983
url https://etheses.whiterose.ac.uk/21743/
https://etheses.whiterose.ac.uk/21743/1/256707.pdf
long_lat ENVELOPE(-83.917,-83.917,-75.917,-75.917)
geographic Siple
geographic_facet Siple
genre Antarc*
Antarctica
Newfoundland
genre_facet Antarc*
Antarctica
Newfoundland
op_relation https://etheses.whiterose.ac.uk/21743/1/256707.pdf
Yearby, Keith Howard (1983) Magnetospheric VLF line radiation. PhD thesis, University of Sheffield.
_version_ 1766253672797306880