Comparative analysis of blind tropospheric correction models in Ghana

The impact of the earth’s atmospheric layers, particularly the troposphere on Global Navigation satellite system (GNSS) signals has become a major concern in GNSS accurate positioning, navigation, surveillance and timing applications. For precise GNSS applications, tropospheric delay has to be mitig...

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Autores principales: Osah S., Acheampong A. A., Fosu C., Dadzie I.
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Publicado: Sciendo 2021
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spelling oai:doaj.org-article:d50de2a0f316499582154555ab88d8cc2021-12-05T14:10:52ZComparative analysis of blind tropospheric correction models in Ghana2081-994310.1515/jogs-2020-0104https://doaj.org/article/d50de2a0f316499582154555ab88d8cc2021-05-01T00:00:00Zhttps://doi.org/10.1515/jogs-2020-0104https://doaj.org/toc/2081-9943The impact of the earth’s atmospheric layers, particularly the troposphere on Global Navigation satellite system (GNSS) signals has become a major concern in GNSS accurate positioning, navigation, surveillance and timing applications. For precise GNSS applications, tropospheric delay has to be mitigated as accurately as possible using tropospheric delay prediction models. However, the choice of a particular prediction model can signifi-cantly impair the positioning accuracy particularly when the model does not suit the user’s environment. A performance assessment of these prediction models for a suitable one is very important. In this paper, an assessment study of the performances of five blind tropospheric delay prediction models, the UNB3m, EGNOS, GTrop, GPT2w and GPT3 models was conducted in Ghana over six selected Continuously Operating Reference Stations (CORS) using the 1˚x1˚ gridded Vienna Mapping Function 3 (VMF3) zenith tropospheric delay (ZTD) product as a reference. The gridded VMF3-ZTD which is generated for every six hours on the 1˚x1˚ grids was bilinearly interpolated both space and time and transferred from the grid heights to the respective heights of the CORS locations. The results show that the GPT3 model performed better in estimating the ZTD with an overall mean (bias: 2.05 cm; RMS: 2.53 cm), followed by GPT2w model (bias: 2.32cm; RMS: 2.76cm) and GTrop model (bias: 2.41cm; 2.82cm). UNB3m model (bias: 6.23 cm; RMS: 6.43 cm) and EGNOS model (bias: 6.70 cm; RMS: 6.89 cm) performed poorly. A multiple comparison test (MCT) was further performed on the RMSE of each model to check if there is significant difference at 5% significant level. The results show that the GPT3, GPT2w and GTrop models are significantly indifferent at 5% significance level indicating that either of these models can be employed to mitigate the ZTD in the study area, nevertheless, the choice of GPT3 model will be more preferable.Osah S.Acheampong A. A.Fosu C.Dadzie I.Sciendoarticlegnssmultiple comparison testprediction modelstropospheric delayvienna mapping functionsGeodesyQB275-343ENJournal of Geodetic Science, Vol 11, Iss 1, Pp 14-26 (2021)
institution DOAJ
collection DOAJ
language EN
topic gnss
multiple comparison test
prediction models
tropospheric delay
vienna mapping functions
Geodesy
QB275-343
spellingShingle gnss
multiple comparison test
prediction models
tropospheric delay
vienna mapping functions
Geodesy
QB275-343
Osah S.
Acheampong A. A.
Fosu C.
Dadzie I.
Comparative analysis of blind tropospheric correction models in Ghana
description The impact of the earth’s atmospheric layers, particularly the troposphere on Global Navigation satellite system (GNSS) signals has become a major concern in GNSS accurate positioning, navigation, surveillance and timing applications. For precise GNSS applications, tropospheric delay has to be mitigated as accurately as possible using tropospheric delay prediction models. However, the choice of a particular prediction model can signifi-cantly impair the positioning accuracy particularly when the model does not suit the user’s environment. A performance assessment of these prediction models for a suitable one is very important. In this paper, an assessment study of the performances of five blind tropospheric delay prediction models, the UNB3m, EGNOS, GTrop, GPT2w and GPT3 models was conducted in Ghana over six selected Continuously Operating Reference Stations (CORS) using the 1˚x1˚ gridded Vienna Mapping Function 3 (VMF3) zenith tropospheric delay (ZTD) product as a reference. The gridded VMF3-ZTD which is generated for every six hours on the 1˚x1˚ grids was bilinearly interpolated both space and time and transferred from the grid heights to the respective heights of the CORS locations. The results show that the GPT3 model performed better in estimating the ZTD with an overall mean (bias: 2.05 cm; RMS: 2.53 cm), followed by GPT2w model (bias: 2.32cm; RMS: 2.76cm) and GTrop model (bias: 2.41cm; 2.82cm). UNB3m model (bias: 6.23 cm; RMS: 6.43 cm) and EGNOS model (bias: 6.70 cm; RMS: 6.89 cm) performed poorly. A multiple comparison test (MCT) was further performed on the RMSE of each model to check if there is significant difference at 5% significant level. The results show that the GPT3, GPT2w and GTrop models are significantly indifferent at 5% significance level indicating that either of these models can be employed to mitigate the ZTD in the study area, nevertheless, the choice of GPT3 model will be more preferable.
format article
author Osah S.
Acheampong A. A.
Fosu C.
Dadzie I.
author_facet Osah S.
Acheampong A. A.
Fosu C.
Dadzie I.
author_sort Osah S.
title Comparative analysis of blind tropospheric correction models in Ghana
title_short Comparative analysis of blind tropospheric correction models in Ghana
title_full Comparative analysis of blind tropospheric correction models in Ghana
title_fullStr Comparative analysis of blind tropospheric correction models in Ghana
title_full_unstemmed Comparative analysis of blind tropospheric correction models in Ghana
title_sort comparative analysis of blind tropospheric correction models in ghana
publisher Sciendo
publishDate 2021
url https://doaj.org/article/d50de2a0f316499582154555ab88d8cc
work_keys_str_mv AT osahs comparativeanalysisofblindtroposphericcorrectionmodelsinghana
AT acheampongaa comparativeanalysisofblindtroposphericcorrectionmodelsinghana
AT fosuc comparativeanalysisofblindtroposphericcorrectionmodelsinghana
AT dadziei comparativeanalysisofblindtroposphericcorrectionmodelsinghana
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