Principal component analysis as a tool to extract Sq variation from the geomagnetic field observations: Conditions of applicability

Bibliographic Details
Main Author: Morozova, A. L.
Publication Date: 2023
Other Authors: Rebbah, Rania
Format: Article
Language: eng
Source: Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)
Download full: https://hdl.handle.net/10316/114804
https://doi.org/10.1016/j.mex.2023.101999
Summary: We analyzed the applicability of the principal component analysis (PCA) as a tool to extract the Sq variation of the geomagnetic field (GMF) taking into account different geomagnetic field components, data measured at different levels of the solar and geomagnetic activity, data from different months. The validation of the method was performed with geomagnetic data obtained at the Coimbra Magnetic Observatory in Portugal (40° 13' N, 8° 25.3' W, 99 m a.s.l., IAGA code COI). GMF variations obtained with PCA were "classified" as SqPCA using reference series: (1) obtained from the observational data (SqIQD), (2) simulated by ionospheric field models. While our results show that both the data-based and model-based reference series can be used, the DIFI3 model performs better as a reference series for GMF at middle latitudes. We also recommend to estimate the similarity of the series with a metric that account for possible local stretching/compressing of the compared series, for example, the dynamic time warping (DTW) distance. Since the validation of the method was performed on the geomagnetic series obtained at a mid-latitudinal European observatory, we recommend performing additional tests when applying this method to data obtained in other regions/latitudes.•For the Y and Z components of the geomagnetic field PCA can be used to extract Sq variations from the observations without any additional procedures and SqPCA is equals to PC1.•For the X component PCA can be used to extract Sq variation from the observations of the X component, but further analysis, for example, a comparison to a set of reference curves either obtained from the data analysis or generated using models, is always needed to classify PCs of the X component.•We recommend to use data generated by DIFI-class models as reference series and the dtw metric (dynamic time warping distance) to classify SqPCA.
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spelling Principal component analysis as a tool to extract Sq variation from the geomagnetic field observations: Conditions of applicabilityPrincipal component analysisGeomagnetic fieldSolar quiet variation (Sq)Coimbra magnetic observatory (COI)We analyzed the applicability of the principal component analysis (PCA) as a tool to extract the Sq variation of the geomagnetic field (GMF) taking into account different geomagnetic field components, data measured at different levels of the solar and geomagnetic activity, data from different months. The validation of the method was performed with geomagnetic data obtained at the Coimbra Magnetic Observatory in Portugal (40° 13' N, 8° 25.3' W, 99 m a.s.l., IAGA code COI). GMF variations obtained with PCA were "classified" as SqPCA using reference series: (1) obtained from the observational data (SqIQD), (2) simulated by ionospheric field models. While our results show that both the data-based and model-based reference series can be used, the DIFI3 model performs better as a reference series for GMF at middle latitudes. We also recommend to estimate the similarity of the series with a metric that account for possible local stretching/compressing of the compared series, for example, the dynamic time warping (DTW) distance. Since the validation of the method was performed on the geomagnetic series obtained at a mid-latitudinal European observatory, we recommend performing additional tests when applying this method to data obtained in other regions/latitudes.•For the Y and Z components of the geomagnetic field PCA can be used to extract Sq variations from the observations without any additional procedures and SqPCA is equals to PC1.•For the X component PCA can be used to extract Sq variation from the observations of the X component, but further analysis, for example, a comparison to a set of reference curves either obtained from the data analysis or generated using models, is always needed to classify PCs of the X component.•We recommend to use data generated by DIFI-class models as reference series and the dtw metric (dynamic time warping distance) to classify SqPCA.Elsevier2023info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttps://hdl.handle.net/10316/114804https://hdl.handle.net/10316/114804https://doi.org/10.1016/j.mex.2023.101999eng2215-0161Morozova, A. L.Rebbah, Raniainfo:eu-repo/semantics/openAccessreponame:Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)instname:FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologiainstacron:RCAAP2024-04-12T09:50:21Zoai:estudogeral.uc.pt:10316/114804Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireinfo@rcaap.ptopendoar:https://opendoar.ac.uk/repository/71602025-05-29T06:08:00.281333Repositórios Científicos de Acesso Aberto de Portugal (RCAAP) - FCCN, serviços digitais da FCT – Fundação para a Ciência e a Tecnologiafalse
dc.title.none.fl_str_mv Principal component analysis as a tool to extract Sq variation from the geomagnetic field observations: Conditions of applicability
title Principal component analysis as a tool to extract Sq variation from the geomagnetic field observations: Conditions of applicability
spellingShingle Principal component analysis as a tool to extract Sq variation from the geomagnetic field observations: Conditions of applicability
Morozova, A. L.
Principal component analysis
Geomagnetic field
Solar quiet variation (Sq)
Coimbra magnetic observatory (COI)
title_short Principal component analysis as a tool to extract Sq variation from the geomagnetic field observations: Conditions of applicability
title_full Principal component analysis as a tool to extract Sq variation from the geomagnetic field observations: Conditions of applicability
title_fullStr Principal component analysis as a tool to extract Sq variation from the geomagnetic field observations: Conditions of applicability
title_full_unstemmed Principal component analysis as a tool to extract Sq variation from the geomagnetic field observations: Conditions of applicability
title_sort Principal component analysis as a tool to extract Sq variation from the geomagnetic field observations: Conditions of applicability
author Morozova, A. L.
author_facet Morozova, A. L.
Rebbah, Rania
author_role author
author2 Rebbah, Rania
author2_role author
dc.contributor.author.fl_str_mv Morozova, A. L.
Rebbah, Rania
dc.subject.por.fl_str_mv Principal component analysis
Geomagnetic field
Solar quiet variation (Sq)
Coimbra magnetic observatory (COI)
topic Principal component analysis
Geomagnetic field
Solar quiet variation (Sq)
Coimbra magnetic observatory (COI)
description We analyzed the applicability of the principal component analysis (PCA) as a tool to extract the Sq variation of the geomagnetic field (GMF) taking into account different geomagnetic field components, data measured at different levels of the solar and geomagnetic activity, data from different months. The validation of the method was performed with geomagnetic data obtained at the Coimbra Magnetic Observatory in Portugal (40° 13' N, 8° 25.3' W, 99 m a.s.l., IAGA code COI). GMF variations obtained with PCA were "classified" as SqPCA using reference series: (1) obtained from the observational data (SqIQD), (2) simulated by ionospheric field models. While our results show that both the data-based and model-based reference series can be used, the DIFI3 model performs better as a reference series for GMF at middle latitudes. We also recommend to estimate the similarity of the series with a metric that account for possible local stretching/compressing of the compared series, for example, the dynamic time warping (DTW) distance. Since the validation of the method was performed on the geomagnetic series obtained at a mid-latitudinal European observatory, we recommend performing additional tests when applying this method to data obtained in other regions/latitudes.•For the Y and Z components of the geomagnetic field PCA can be used to extract Sq variations from the observations without any additional procedures and SqPCA is equals to PC1.•For the X component PCA can be used to extract Sq variation from the observations of the X component, but further analysis, for example, a comparison to a set of reference curves either obtained from the data analysis or generated using models, is always needed to classify PCs of the X component.•We recommend to use data generated by DIFI-class models as reference series and the dtw metric (dynamic time warping distance) to classify SqPCA.
publishDate 2023
dc.date.none.fl_str_mv 2023
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
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dc.identifier.uri.fl_str_mv https://hdl.handle.net/10316/114804
https://hdl.handle.net/10316/114804
https://doi.org/10.1016/j.mex.2023.101999
url https://hdl.handle.net/10316/114804
https://doi.org/10.1016/j.mex.2023.101999
dc.language.iso.fl_str_mv eng
language eng
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dc.publisher.none.fl_str_mv Elsevier
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collection Repositórios Científicos de Acesso Aberto de Portugal (RCAAP)
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