Medium-scale 4-D ionospheric tomography using a dense GPS network

The ionosphere above Scandinavia in December 2006 is successfully imaged by 4-dimensional tomography using the software package MIDAS from the University of Bath. The method concentrates on medium-scale structures: between 100 km and 2000 km in horizontal size. The input consists of TEC measurem...

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Main Author: M. M. J. L. van de Kamp
Format: Article
Language:English
Published: Copernicus Publications 2013-01-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/31/75/2013/angeo-31-75-2013.pdf
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spelling doaj-cb8259f24b7740c09401cd9edcad570e2020-11-24T21:11:13ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762013-01-0131758910.5194/angeo-31-75-2013Medium-scale 4-D ionospheric tomography using a dense GPS networkM. M. J. L. van de Kamp0Finnish Meteorological Institute, P.O. Box 503, 00101 Helsinki, FinlandThe ionosphere above Scandinavia in December 2006 is successfully imaged by 4-dimensional tomography using the software package MIDAS from the University of Bath. The method concentrates on medium-scale structures: between 100 km and 2000 km in horizontal size. The input consists of TEC measurements from the dense GPS network Geotrim in Finland. In order to ensure sufficient vertical resolution of the result, EISCAT incoherent scatter radar data from Tromsø are used as additional input to provide the vertical profile information. <br><br> The TEC offset of the measurements is unknown, but the inversion procedure is able to determine this automatically. This auto-calibration is shown to work well. <br><br> Comparisons with EISCAT radar results and with occultation results show that the inversion using EISCAT data for profile information is much better able to resolve vertical profiles of irregular structures than the inversion using built-in profiles. Still, with either method the intensities of irregular structures of sizes near the resolution (about 100 km horizontal size) can be underestimated. Also, the accuracy of the inversion worsens above areas where no receivers are available. <br><br> The ionosphere over Scandinavia in December 2006 often showed a dense E-layer in early morning hours, which generally disappeared during midday when a dense F-layer was present. On 14 December, a strong coronal mass ejection occurred, and many intense irregularities appeared in the ionosphere, which extended to high altitudes.https://www.ann-geophys.net/31/75/2013/angeo-31-75-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. M. J. L. van de Kamp
spellingShingle M. M. J. L. van de Kamp
Medium-scale 4-D ionospheric tomography using a dense GPS network
Annales Geophysicae
author_facet M. M. J. L. van de Kamp
author_sort M. M. J. L. van de Kamp
title Medium-scale 4-D ionospheric tomography using a dense GPS network
title_short Medium-scale 4-D ionospheric tomography using a dense GPS network
title_full Medium-scale 4-D ionospheric tomography using a dense GPS network
title_fullStr Medium-scale 4-D ionospheric tomography using a dense GPS network
title_full_unstemmed Medium-scale 4-D ionospheric tomography using a dense GPS network
title_sort medium-scale 4-d ionospheric tomography using a dense gps network
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2013-01-01
description The ionosphere above Scandinavia in December 2006 is successfully imaged by 4-dimensional tomography using the software package MIDAS from the University of Bath. The method concentrates on medium-scale structures: between 100 km and 2000 km in horizontal size. The input consists of TEC measurements from the dense GPS network Geotrim in Finland. In order to ensure sufficient vertical resolution of the result, EISCAT incoherent scatter radar data from Tromsø are used as additional input to provide the vertical profile information. <br><br> The TEC offset of the measurements is unknown, but the inversion procedure is able to determine this automatically. This auto-calibration is shown to work well. <br><br> Comparisons with EISCAT radar results and with occultation results show that the inversion using EISCAT data for profile information is much better able to resolve vertical profiles of irregular structures than the inversion using built-in profiles. Still, with either method the intensities of irregular structures of sizes near the resolution (about 100 km horizontal size) can be underestimated. Also, the accuracy of the inversion worsens above areas where no receivers are available. <br><br> The ionosphere over Scandinavia in December 2006 often showed a dense E-layer in early morning hours, which generally disappeared during midday when a dense F-layer was present. On 14 December, a strong coronal mass ejection occurred, and many intense irregularities appeared in the ionosphere, which extended to high altitudes.
url https://www.ann-geophys.net/31/75/2013/angeo-31-75-2013.pdf
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