Planetary and gravity wave signatures in the F-region ionosphere with impacton radio propagation predictionsand variability

The aim of this work within the WP 3.1 of the COST 271 Action is the characterization of the variability introduced in the F-region ionosphere by -Planetary Wave Signatures- (PWS) and -Gravity Wave Signatures- (GWS). Typical patterns of percentage of time occurrence and time duration of PWS, their c...

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Main Authors: P. Sauli, J. Lastovicka, J. Boska, E. M. Apostolov, D. Altadill
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2004-06-01
Series:Annals of Geophysics
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/3288
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spelling doaj-3eef795675ad47359cc39bc7579242da2020-11-24T22:52:39ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2004-06-01472-3 Sup.10.4401/ag-3288Planetary and gravity wave signatures in the F-region ionosphere with impacton radio propagation predictionsand variabilityP. SauliJ. LastovickaJ. BoskaE. M. ApostolovD. AltadillThe aim of this work within the WP 3.1 of the COST 271 Action is the characterization of the variability introduced in the F-region ionosphere by -Planetary Wave Signatures- (PWS) and -Gravity Wave Signatures- (GWS). Typical patterns of percentage of time occurrence and time duration of PWS, their climatology and main drivers, as well as their vertical and longitudinal structure have been obtained. Despite the above characterization, the spectral distribution of event duration is too broad to allow for a reasonable prediction of PWS from ionospheric measurements themselves. GWS with a regular morning/evening wave bursts and specific GWS events whose arising can be predicted have been evaluated. As above, their typical pattern of occurrence and time duration, and their vertical structure have been obtained. The latter events remain in the ionospheric variability during disturbed days while additional wave enhancements of auroral origin occur. However, both types of disturbances can be distinguished.http://www.annalsofgeophysics.eu/index.php/annals/article/view/3288
collection DOAJ
language English
format Article
sources DOAJ
author P. Sauli
J. Lastovicka
J. Boska
E. M. Apostolov
D. Altadill
spellingShingle P. Sauli
J. Lastovicka
J. Boska
E. M. Apostolov
D. Altadill
Planetary and gravity wave signatures in the F-region ionosphere with impacton radio propagation predictionsand variability
Annals of Geophysics
author_facet P. Sauli
J. Lastovicka
J. Boska
E. M. Apostolov
D. Altadill
author_sort P. Sauli
title Planetary and gravity wave signatures in the F-region ionosphere with impacton radio propagation predictionsand variability
title_short Planetary and gravity wave signatures in the F-region ionosphere with impacton radio propagation predictionsand variability
title_full Planetary and gravity wave signatures in the F-region ionosphere with impacton radio propagation predictionsand variability
title_fullStr Planetary and gravity wave signatures in the F-region ionosphere with impacton radio propagation predictionsand variability
title_full_unstemmed Planetary and gravity wave signatures in the F-region ionosphere with impacton radio propagation predictionsand variability
title_sort planetary and gravity wave signatures in the f-region ionosphere with impacton radio propagation predictionsand variability
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 2004-06-01
description The aim of this work within the WP 3.1 of the COST 271 Action is the characterization of the variability introduced in the F-region ionosphere by -Planetary Wave Signatures- (PWS) and -Gravity Wave Signatures- (GWS). Typical patterns of percentage of time occurrence and time duration of PWS, their climatology and main drivers, as well as their vertical and longitudinal structure have been obtained. Despite the above characterization, the spectral distribution of event duration is too broad to allow for a reasonable prediction of PWS from ionospheric measurements themselves. GWS with a regular morning/evening wave bursts and specific GWS events whose arising can be predicted have been evaluated. As above, their typical pattern of occurrence and time duration, and their vertical structure have been obtained. The latter events remain in the ionospheric variability during disturbed days while additional wave enhancements of auroral origin occur. However, both types of disturbances can be distinguished.
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/3288
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AT emapostolov planetaryandgravitywavesignaturesinthefregionionospherewithimpactonradiopropagationpredictionsandvariability
AT daltadill planetaryandgravitywavesignaturesinthefregionionospherewithimpactonradiopropagationpredictionsandvariability
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