Introduction of new data into the South African Ionospheric Map to improve the estimation of F2 layer parameters

<p>In this paper the South African Ionospheric Map (SAIM) is upgraded with the usage of recent International Reference Ionosphere (IRI)-2012 model and South African Bottomside Model (SABIM) version 5 and validated for the critical frequency (foF2) of the F2 layer by comparing the model’s outpu...

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Main Authors: Nicholas Ssessanga, Lee-Anne McKinnell, John Bosco Habarulema
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2015-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/6704
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spelling doaj-602f76248d8e4fc0ae668571d2e691132020-11-25T01:28:37ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2015-06-0158210.4401/ag-67046027Introduction of new data into the South African Ionospheric Map to improve the estimation of F2 layer parametersNicholas Ssessanga0Lee-Anne McKinnell1John Bosco Habarulema2Chunganam National University (CNU), Department of Astronomy and Space Science, Daejeon,South African National Space Agency (SANSA) Space Science, Hermanus,South African National Space Agency (SANSA) Space Science, Hermanus,<p>In this paper the South African Ionospheric Map (SAIM) is upgraded with the usage of recent International Reference Ionosphere (IRI)-2012 model and South African Bottomside Model (SABIM) version 5 and validated for the critical frequency (foF2) of the F2 layer by comparing the model’s output with the measured ionosonde data. The SABIM model is also validated before use in the SAIM. The ionosonde stations used in the analysis include; Grahamstown (33.2°S, 26.3°E), Hermanus (34.4°S, 19.2°E), Louisvale (28.5°S, 21.2°E) and Madimbo (22.4°S, 30.9°E). The analysis of the results showed that the updates improved the performance of SAIM by 75% over the first version. The foF2 estimates from the SABIM version 5 model also gave a better estimate to the ionosonde measurements compared to the IRI-2012 model. The SABIM model performed 27% better than the IRI-2012 model during solar maximum and 14.7% better during solar minimum.</p>http://www.annalsofgeophysics.eu/index.php/annals/article/view/6704South African Ionospheric Map (SAIM)F2 layer critical frequency (foF2)
collection DOAJ
language English
format Article
sources DOAJ
author Nicholas Ssessanga
Lee-Anne McKinnell
John Bosco Habarulema
spellingShingle Nicholas Ssessanga
Lee-Anne McKinnell
John Bosco Habarulema
Introduction of new data into the South African Ionospheric Map to improve the estimation of F2 layer parameters
Annals of Geophysics
South African Ionospheric Map (SAIM)
F2 layer critical frequency (foF2)
author_facet Nicholas Ssessanga
Lee-Anne McKinnell
John Bosco Habarulema
author_sort Nicholas Ssessanga
title Introduction of new data into the South African Ionospheric Map to improve the estimation of F2 layer parameters
title_short Introduction of new data into the South African Ionospheric Map to improve the estimation of F2 layer parameters
title_full Introduction of new data into the South African Ionospheric Map to improve the estimation of F2 layer parameters
title_fullStr Introduction of new data into the South African Ionospheric Map to improve the estimation of F2 layer parameters
title_full_unstemmed Introduction of new data into the South African Ionospheric Map to improve the estimation of F2 layer parameters
title_sort introduction of new data into the south african ionospheric map to improve the estimation of f2 layer parameters
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 2015-06-01
description <p>In this paper the South African Ionospheric Map (SAIM) is upgraded with the usage of recent International Reference Ionosphere (IRI)-2012 model and South African Bottomside Model (SABIM) version 5 and validated for the critical frequency (foF2) of the F2 layer by comparing the model’s output with the measured ionosonde data. The SABIM model is also validated before use in the SAIM. The ionosonde stations used in the analysis include; Grahamstown (33.2°S, 26.3°E), Hermanus (34.4°S, 19.2°E), Louisvale (28.5°S, 21.2°E) and Madimbo (22.4°S, 30.9°E). The analysis of the results showed that the updates improved the performance of SAIM by 75% over the first version. The foF2 estimates from the SABIM version 5 model also gave a better estimate to the ionosonde measurements compared to the IRI-2012 model. The SABIM model performed 27% better than the IRI-2012 model during solar maximum and 14.7% better during solar minimum.</p>
topic South African Ionospheric Map (SAIM)
F2 layer critical frequency (foF2)
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/6704
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