Remote sensing planetary waves in the midlatitude mesosphere using low frequency transmitter signals

Very low and low radio frequency (VLF/LF) propagation responds sensitively to the electron density distribution in the lower ionosphere (upper mesosphere). Whereas propagation paths crossing subpolar and polar regions are frequently affected by forcing from above by particle precipitations, mid-...

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Main Author: E. D. Schmitter
Format: Article
Language:English
Published: Copernicus Publications 2011-07-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/29/1287/2011/angeo-29-1287-2011.pdf
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spelling doaj-382ca36d85c8444a83abcaea28cbff6b2020-11-25T01:36:43ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762011-07-01291287129310.5194/angeo-29-1287-2011Remote sensing planetary waves in the midlatitude mesosphere using low frequency transmitter signalsE. D. Schmitter0University of Applied Sciences Osnabrueck, 49076 Osnabrueck, GermanyVery low and low radio frequency (VLF/LF) propagation responds sensitively to the electron density distribution in the lower ionosphere (upper mesosphere). Whereas propagation paths crossing subpolar and polar regions are frequently affected by forcing from above by particle precipitations, mid- and lowlatitude paths let forcing from below be more prominent. Our observations (2009–2011) show, that the low frequency propagation conditions along the midlatitude path from Sicily to Germany (52° N 8° E) using the NSY 45.9 kHz transmitter (37° N 14° E) prove to be a good proxy of mesosphere planetary wave activity along the propagation path. High absorption events with VLF/LF propagation correlate to the well known winter time D-layer anomaly observed with high frequency (HF) radio waves. VLF/LF propagation calculations are presented which show that the radio signal amplitude variations can be modeled by planetary wave modulated collison frequency and electron density profiles. The other way around wave pressure amplitudes can be inferred from the VLF/LF data.https://www.ann-geophys.net/29/1287/2011/angeo-29-1287-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author E. D. Schmitter
spellingShingle E. D. Schmitter
Remote sensing planetary waves in the midlatitude mesosphere using low frequency transmitter signals
Annales Geophysicae
author_facet E. D. Schmitter
author_sort E. D. Schmitter
title Remote sensing planetary waves in the midlatitude mesosphere using low frequency transmitter signals
title_short Remote sensing planetary waves in the midlatitude mesosphere using low frequency transmitter signals
title_full Remote sensing planetary waves in the midlatitude mesosphere using low frequency transmitter signals
title_fullStr Remote sensing planetary waves in the midlatitude mesosphere using low frequency transmitter signals
title_full_unstemmed Remote sensing planetary waves in the midlatitude mesosphere using low frequency transmitter signals
title_sort remote sensing planetary waves in the midlatitude mesosphere using low frequency transmitter signals
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2011-07-01
description Very low and low radio frequency (VLF/LF) propagation responds sensitively to the electron density distribution in the lower ionosphere (upper mesosphere). Whereas propagation paths crossing subpolar and polar regions are frequently affected by forcing from above by particle precipitations, mid- and lowlatitude paths let forcing from below be more prominent. Our observations (2009–2011) show, that the low frequency propagation conditions along the midlatitude path from Sicily to Germany (52° N 8° E) using the NSY 45.9 kHz transmitter (37° N 14° E) prove to be a good proxy of mesosphere planetary wave activity along the propagation path. High absorption events with VLF/LF propagation correlate to the well known winter time D-layer anomaly observed with high frequency (HF) radio waves. VLF/LF propagation calculations are presented which show that the radio signal amplitude variations can be modeled by planetary wave modulated collison frequency and electron density profiles. The other way around wave pressure amplitudes can be inferred from the VLF/LF data.
url https://www.ann-geophys.net/29/1287/2011/angeo-29-1287-2011.pdf
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