Fractal Dimension Analysis of Earth Magnetic Field during 26 August 2018 Geomagnetic Storm

We analyse the fractal nature of geomagnetic field northward and eastward horizontal components with 1 min resolution measured by the four stations Belsk, Hel, Sodankylä and Hornsund during the period of 22 August–1 September, when the 26 August 2018 geomagnetic storm appeared. To reveal and to quan...

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Published in:Entropy
Main Authors: Anna Wawrzaszek, Renata Modzelewska, Agata Krasińska, Agnieszka Gil, Vasile Glavan
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
Subjects:
Online Access:https://doi.org/10.3390/e24050699
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author Anna Wawrzaszek
Renata Modzelewska
Agata Krasińska
Agnieszka Gil
Vasile Glavan
author_facet Anna Wawrzaszek
Renata Modzelewska
Agata Krasińska
Agnieszka Gil
Vasile Glavan
author_sort Anna Wawrzaszek
collection MDPI Open Access Publishing
container_issue 5
container_start_page 699
container_title Entropy
container_volume 24
description We analyse the fractal nature of geomagnetic field northward and eastward horizontal components with 1 min resolution measured by the four stations Belsk, Hel, Sodankylä and Hornsund during the period of 22 August–1 September, when the 26 August 2018 geomagnetic storm appeared. To reveal and to quantitatively describe the fractal scaling of the considered data, three selected methods, structure function scaling, Higuchi, and detrended fluctuation analysis are applied. The obtained results show temporal variation of the fractal dimension of geomagnetic field components, revealing differences between their irregularity (complexity). The values of fractal dimension seem to be sensitive to the physical conditions connected with the interplanetary shock, the coronal mass ejection, the corotating interaction region, and the high-speed stream passage during the storm development. Especially, just after interplanetary shock occurrence, a decrease in the fractal dimension for all stations is observed, not straightforwardly visible in the geomagnetic field components data.
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genre Hornsund
Sodankylä
genre_facet Hornsund
Sodankylä
geographic Hornsund
Sodankylä
geographic_facet Hornsund
Sodankylä
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long_lat ENVELOPE(15.865,15.865,76.979,76.979)
ENVELOPE(26.600,26.600,67.417,67.417)
op_collection_id ftmdpi
op_doi https://doi.org/10.3390/e24050699
op_relation https://dx.doi.org/10.3390/e24050699
op_rights https://creativecommons.org/licenses/by/4.0/
op_source Entropy; Volume 24; Issue 5; Pages: 699
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spelling ftmdpi:oai:mdpi.com:/1099-4300/24/5/699/ 2025-01-16T22:19:03+00:00 Fractal Dimension Analysis of Earth Magnetic Field during 26 August 2018 Geomagnetic Storm Anna Wawrzaszek Renata Modzelewska Agata Krasińska Agnieszka Gil Vasile Glavan 2022-05-14 application/pdf https://doi.org/10.3390/e24050699 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/e24050699 https://creativecommons.org/licenses/by/4.0/ Entropy; Volume 24; Issue 5; Pages: 699 fractal dimension time series geomagnetic field geomagnetic storms Text 2022 ftmdpi https://doi.org/10.3390/e24050699 2023-08-01T05:03:20Z We analyse the fractal nature of geomagnetic field northward and eastward horizontal components with 1 min resolution measured by the four stations Belsk, Hel, Sodankylä and Hornsund during the period of 22 August–1 September, when the 26 August 2018 geomagnetic storm appeared. To reveal and to quantitatively describe the fractal scaling of the considered data, three selected methods, structure function scaling, Higuchi, and detrended fluctuation analysis are applied. The obtained results show temporal variation of the fractal dimension of geomagnetic field components, revealing differences between their irregularity (complexity). The values of fractal dimension seem to be sensitive to the physical conditions connected with the interplanetary shock, the coronal mass ejection, the corotating interaction region, and the high-speed stream passage during the storm development. Especially, just after interplanetary shock occurrence, a decrease in the fractal dimension for all stations is observed, not straightforwardly visible in the geomagnetic field components data. Text Hornsund Sodankylä MDPI Open Access Publishing Hornsund ENVELOPE(15.865,15.865,76.979,76.979) Sodankylä ENVELOPE(26.600,26.600,67.417,67.417) Entropy 24 5 699
spellingShingle fractal dimension
time series
geomagnetic field
geomagnetic storms
Anna Wawrzaszek
Renata Modzelewska
Agata Krasińska
Agnieszka Gil
Vasile Glavan
Fractal Dimension Analysis of Earth Magnetic Field during 26 August 2018 Geomagnetic Storm
title Fractal Dimension Analysis of Earth Magnetic Field during 26 August 2018 Geomagnetic Storm
title_full Fractal Dimension Analysis of Earth Magnetic Field during 26 August 2018 Geomagnetic Storm
title_fullStr Fractal Dimension Analysis of Earth Magnetic Field during 26 August 2018 Geomagnetic Storm
title_full_unstemmed Fractal Dimension Analysis of Earth Magnetic Field during 26 August 2018 Geomagnetic Storm
title_short Fractal Dimension Analysis of Earth Magnetic Field during 26 August 2018 Geomagnetic Storm
title_sort fractal dimension analysis of earth magnetic field during 26 august 2018 geomagnetic storm
topic fractal dimension
time series
geomagnetic field
geomagnetic storms
topic_facet fractal dimension
time series
geomagnetic field
geomagnetic storms
url https://doi.org/10.3390/e24050699