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The ionospheric irregularities climatology over Svalbard from solar cycle 23

The paper presents an unprecedented description of the climatology of ionospheric irregularities over the Arctic derived from the longest Global Navigation Satellite Systems data series ever collected for this specific aim. Two TEC and scintillation receivers are working at Ny-Ålesund (Svalbard, NO)...

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Autores principales: De Franceschi, Giorgiana, Spogli, Luca, Alfonsi, Lucilla, Romano, Vincenzo, Cesaroni, Claudio, Hunstad, Ingrid
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6592953/
https://www.ncbi.nlm.nih.gov/pubmed/31239449
http://dx.doi.org/10.1038/s41598-019-44829-5
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author De Franceschi, Giorgiana
Spogli, Luca
Alfonsi, Lucilla
Romano, Vincenzo
Cesaroni, Claudio
Hunstad, Ingrid
author_facet De Franceschi, Giorgiana
Spogli, Luca
Alfonsi, Lucilla
Romano, Vincenzo
Cesaroni, Claudio
Hunstad, Ingrid
author_sort De Franceschi, Giorgiana
collection PubMed
description The paper presents an unprecedented description of the climatology of ionospheric irregularities over the Arctic derived from the longest Global Navigation Satellite Systems data series ever collected for this specific aim. Two TEC and scintillation receivers are working at Ny-Ålesund (Svalbard, NO), the first of which has been installed in late September 2003. They sample the L1 and L2 signals at 50 Hz from all the GPS satellites in view. The receivers monitor an area of about 600 km radius that includes the auroral and cusp/cap regions in the European longitudinal sector. The length of the data series and the privileged site of observation allow describing the Arctic ionosphere along about two solar cycles, from the descending phase of cycle 23 to almost the end of cycle 24. Our analysis results into a detailed assessment of the long-term behaviour of the ionosphere under solar maximum and solar minimum conditions, including several periods of perturbed ionospheric weather caused by unfavourable helio-geophysical conditions. Since November 2015, a multi-constellation GNSS receiver has been deployed in Ny-Ålesund, providing the opportunity to perform the ionospheric climatology from Galileo signals. The results offer realistic features of the high latitude ionosphere that can substantially contribute to the necessary improvements of forecasting models, providing a broad spectrum of ionospheric reactions to different space weather conditions.
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spelling pubmed-65929532019-07-03 The ionospheric irregularities climatology over Svalbard from solar cycle 23 De Franceschi, Giorgiana Spogli, Luca Alfonsi, Lucilla Romano, Vincenzo Cesaroni, Claudio Hunstad, Ingrid Sci Rep Article The paper presents an unprecedented description of the climatology of ionospheric irregularities over the Arctic derived from the longest Global Navigation Satellite Systems data series ever collected for this specific aim. Two TEC and scintillation receivers are working at Ny-Ålesund (Svalbard, NO), the first of which has been installed in late September 2003. They sample the L1 and L2 signals at 50 Hz from all the GPS satellites in view. The receivers monitor an area of about 600 km radius that includes the auroral and cusp/cap regions in the European longitudinal sector. The length of the data series and the privileged site of observation allow describing the Arctic ionosphere along about two solar cycles, from the descending phase of cycle 23 to almost the end of cycle 24. Our analysis results into a detailed assessment of the long-term behaviour of the ionosphere under solar maximum and solar minimum conditions, including several periods of perturbed ionospheric weather caused by unfavourable helio-geophysical conditions. Since November 2015, a multi-constellation GNSS receiver has been deployed in Ny-Ålesund, providing the opportunity to perform the ionospheric climatology from Galileo signals. The results offer realistic features of the high latitude ionosphere that can substantially contribute to the necessary improvements of forecasting models, providing a broad spectrum of ionospheric reactions to different space weather conditions. Nature Publishing Group UK 2019-06-25 /pmc/articles/PMC6592953/ /pubmed/31239449 http://dx.doi.org/10.1038/s41598-019-44829-5 Text en © The Author(s) 2019 Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.
spellingShingle Article
De Franceschi, Giorgiana
Spogli, Luca
Alfonsi, Lucilla
Romano, Vincenzo
Cesaroni, Claudio
Hunstad, Ingrid
The ionospheric irregularities climatology over Svalbard from solar cycle 23
title The ionospheric irregularities climatology over Svalbard from solar cycle 23
title_full The ionospheric irregularities climatology over Svalbard from solar cycle 23
title_fullStr The ionospheric irregularities climatology over Svalbard from solar cycle 23
title_full_unstemmed The ionospheric irregularities climatology over Svalbard from solar cycle 23
title_short The ionospheric irregularities climatology over Svalbard from solar cycle 23
title_sort ionospheric irregularities climatology over svalbard from solar cycle 23
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6592953/
https://www.ncbi.nlm.nih.gov/pubmed/31239449
http://dx.doi.org/10.1038/s41598-019-44829-5
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