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...
Published in: | Entropy |
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Main Authors: | , , , , |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2022
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Subjects: | |
Online Access: | https://doi.org/10.3390/e24050699 |
_version_ | 1821536635195490304 |
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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. |
format | Text |
genre | Hornsund Sodankylä |
genre_facet | Hornsund Sodankylä |
geographic | Hornsund Sodankylä |
geographic_facet | Hornsund Sodankylä |
id | ftmdpi:oai:mdpi.com:/1099-4300/24/5/699/ |
institution | Open Polar |
language | English |
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 |
publishDate | 2022 |
publisher | Multidisciplinary Digital Publishing Institute |
record_format | openpolar |
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 |