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 measurements...

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Published in:Annales Geophysicae
Main Author: Kamp, M. M. J. L.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/angeo-31-75-2013
https://angeo.copernicus.org/articles/31/75/2013/
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spelling ftcopernicus:oai:publications.copernicus.org:angeo13794 2023-05-15T16:04:29+02:00 Medium-scale 4-D ionospheric tomography using a dense GPS network Kamp, M. M. J. L. 2018-09-27 application/pdf https://doi.org/10.5194/angeo-31-75-2013 https://angeo.copernicus.org/articles/31/75/2013/ eng eng doi:10.5194/angeo-31-75-2013 https://angeo.copernicus.org/articles/31/75/2013/ eISSN: 1432-0576 Text 2018 ftcopernicus https://doi.org/10.5194/angeo-31-75-2013 2020-07-20T16:25:35Z 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. 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. 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. 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. Text EISCAT Tromsø Copernicus Publications: E-Journals Tromsø Annales Geophysicae 31 1 75 89
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
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. 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. 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. 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.
format Text
author Kamp, M. M. J. L.
spellingShingle Kamp, M. M. J. L.
Medium-scale 4-D ionospheric tomography using a dense GPS network
author_facet Kamp, M. M. J. L.
author_sort Kamp, M. M. J. L.
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
publishDate 2018
url https://doi.org/10.5194/angeo-31-75-2013
https://angeo.copernicus.org/articles/31/75/2013/
geographic Tromsø
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genre_facet EISCAT
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op_source eISSN: 1432-0576
op_relation doi:10.5194/angeo-31-75-2013
https://angeo.copernicus.org/articles/31/75/2013/
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container_title Annales Geophysicae
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