A single-station empirical TEC model based on long-time recorded GPS data for estimating ionospheric delay

Globally distributed GPS (global positioning system) stations have been continuously running for nearly 20 years, thereby accumulating numerous observations. These long-time recorded GPS data can be used to calculate continuous total electron content (TEC) values at single stations and provide an ef...

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Main Authors: Zhao Zhenzhen, Feng Jiandi, Han Baomin, Wang Zhengtao
Format: Article
Language:English
Published: EDP Sciences 2018-01-01
Series:Journal of Space Weather and Space Climate
Subjects:
Online Access:https://doi.org/10.1051/swsc/2018047
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spelling doaj-572600daa7e24fc88dfdb6632929e6762021-04-02T15:11:15ZengEDP SciencesJournal of Space Weather and Space Climate2115-72512018-01-018A5910.1051/swsc/2018047swsc180042A single-station empirical TEC model based on long-time recorded GPS data for estimating ionospheric delayZhao ZhenzhenFeng JiandiHan BaominWang ZhengtaoGlobally distributed GPS (global positioning system) stations have been continuously running for nearly 20 years, thereby accumulating numerous observations. These long-time recorded GPS data can be used to calculate continuous total electron content (TEC) values at single stations and provide an effective modeling dataset to establish single-station empirical TEC models. In this paper, a new empirical TEC model called SSM-T1 for single stations is proposed on the basis of GPS data calculated by IONOLAB-TEC application from 2004 to 2015. The SSM-T1 model consists of three parts: diurnal, seasonal, and solar dependency variations, with 18 coefficients fitted by the nonlinear least-squares method. The SSM-T1 model is tested at four stations: Paris (opmt), France; Bangalore (iisc), India; Ceduna (cedu), Australia; and O’Higgins (ohi3) over the Antarctic Peninsula. The RMS values of the model residuals at these four stations are 3.22, 4.46, 3.28, and 3.83 TECU. Assessment results show that the SSM-T1 model is in good agreement with the observed GPS-TEC data and exhibits good prediction ability at the Paris, Bangalore, and Ceduna stations. However, at the O’Higgins station, the SSM-T1 model seriously deviates from the observed GPS-TEC data and cannot effectively describe the variation of mid-latitude summer night anomaly.https://doi.org/10.1051/swsc/2018047empirical TEC modelsionospheric delaysingle stationGPS data
collection DOAJ
language English
format Article
sources DOAJ
author Zhao Zhenzhen
Feng Jiandi
Han Baomin
Wang Zhengtao
spellingShingle Zhao Zhenzhen
Feng Jiandi
Han Baomin
Wang Zhengtao
A single-station empirical TEC model based on long-time recorded GPS data for estimating ionospheric delay
Journal of Space Weather and Space Climate
empirical TEC models
ionospheric delay
single station
GPS data
author_facet Zhao Zhenzhen
Feng Jiandi
Han Baomin
Wang Zhengtao
author_sort Zhao Zhenzhen
title A single-station empirical TEC model based on long-time recorded GPS data for estimating ionospheric delay
title_short A single-station empirical TEC model based on long-time recorded GPS data for estimating ionospheric delay
title_full A single-station empirical TEC model based on long-time recorded GPS data for estimating ionospheric delay
title_fullStr A single-station empirical TEC model based on long-time recorded GPS data for estimating ionospheric delay
title_full_unstemmed A single-station empirical TEC model based on long-time recorded GPS data for estimating ionospheric delay
title_sort single-station empirical tec model based on long-time recorded gps data for estimating ionospheric delay
publisher EDP Sciences
series Journal of Space Weather and Space Climate
issn 2115-7251
publishDate 2018-01-01
description Globally distributed GPS (global positioning system) stations have been continuously running for nearly 20 years, thereby accumulating numerous observations. These long-time recorded GPS data can be used to calculate continuous total electron content (TEC) values at single stations and provide an effective modeling dataset to establish single-station empirical TEC models. In this paper, a new empirical TEC model called SSM-T1 for single stations is proposed on the basis of GPS data calculated by IONOLAB-TEC application from 2004 to 2015. The SSM-T1 model consists of three parts: diurnal, seasonal, and solar dependency variations, with 18 coefficients fitted by the nonlinear least-squares method. The SSM-T1 model is tested at four stations: Paris (opmt), France; Bangalore (iisc), India; Ceduna (cedu), Australia; and O’Higgins (ohi3) over the Antarctic Peninsula. The RMS values of the model residuals at these four stations are 3.22, 4.46, 3.28, and 3.83 TECU. Assessment results show that the SSM-T1 model is in good agreement with the observed GPS-TEC data and exhibits good prediction ability at the Paris, Bangalore, and Ceduna stations. However, at the O’Higgins station, the SSM-T1 model seriously deviates from the observed GPS-TEC data and cannot effectively describe the variation of mid-latitude summer night anomaly.
topic empirical TEC models
ionospheric delay
single station
GPS data
url https://doi.org/10.1051/swsc/2018047
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