Superposed epoch analysis of ground dB/dt variations during shock-induced substorms: The role of shock inclination

A recent case study showed that shock impact angles control the generation of dB/dt variations on the ground during subsequently triggered substorms. More specifically, nearly frontal shocks tend to trigger fast and intense substorms associated with high-level dB/dt variations. On the other hand, hi...

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Main Authors: Oliveira, D., Weygand, J., Delano, K., Zesta, E.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020489
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spelling ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5020489 2023-07-30T04:03:54+02:00 Superposed epoch analysis of ground dB/dt variations during shock-induced substorms: The role of shock inclination Oliveira, D. Weygand, J. Delano, K. Zesta, E. 2023-07-11 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020489 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-3574 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020489 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-3574 2023-07-09T23:40:17Z A recent case study showed that shock impact angles control the generation of dB/dt variations on the ground during subsequently triggered substorms. More specifically, nearly frontal shocks tend to trigger fast and intense substorms associated with high-level dB/dt variations. On the other hand, highly inclined shocks tend to trigger slow and less intense substorms leading to low-level dB/dt variations. In this study, we use a ground magnetometer network with stations located in North America, from western Alaska to eastern Labrador (THEMIS/GMAG) and northwestern Greenland (Technical University of Denmark) to perform a statistical analysis of shock-related dB/dt variations during substorms with an updated shock list containing nearly 600 events. By using the well-known Spherical Elementary Current System (SEC) technique applied to ground magnetometer data, we construct geographical maps with dB/dt variations during the substorms and correlate these variations with shock impact angle as a function of MLATs and MLTs. We find that intense SECs and dB/dt variations occur in larger MLAT bandwidths for the more frontal shocks. By looking at specific MLTs associated with substorm activity, namely MLT > 21 hrs or MLT < 3 hrs around the magnetic midnight, we conclude that nearly frontal shocks indeed cause more intense dB/dt variations that cover wider geographic areas in comparison to highly inclined shocks. These results confirm previous observations of comparative studies and have profound implications to further space weather predictions and forecasting. Conference Object Greenland Alaska GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Greenland
institution Open Polar
collection GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam)
op_collection_id ftgfzpotsdam
language English
description A recent case study showed that shock impact angles control the generation of dB/dt variations on the ground during subsequently triggered substorms. More specifically, nearly frontal shocks tend to trigger fast and intense substorms associated with high-level dB/dt variations. On the other hand, highly inclined shocks tend to trigger slow and less intense substorms leading to low-level dB/dt variations. In this study, we use a ground magnetometer network with stations located in North America, from western Alaska to eastern Labrador (THEMIS/GMAG) and northwestern Greenland (Technical University of Denmark) to perform a statistical analysis of shock-related dB/dt variations during substorms with an updated shock list containing nearly 600 events. By using the well-known Spherical Elementary Current System (SEC) technique applied to ground magnetometer data, we construct geographical maps with dB/dt variations during the substorms and correlate these variations with shock impact angle as a function of MLATs and MLTs. We find that intense SECs and dB/dt variations occur in larger MLAT bandwidths for the more frontal shocks. By looking at specific MLTs associated with substorm activity, namely MLT > 21 hrs or MLT < 3 hrs around the magnetic midnight, we conclude that nearly frontal shocks indeed cause more intense dB/dt variations that cover wider geographic areas in comparison to highly inclined shocks. These results confirm previous observations of comparative studies and have profound implications to further space weather predictions and forecasting.
format Conference Object
author Oliveira, D.
Weygand, J.
Delano, K.
Zesta, E.
spellingShingle Oliveira, D.
Weygand, J.
Delano, K.
Zesta, E.
Superposed epoch analysis of ground dB/dt variations during shock-induced substorms: The role of shock inclination
author_facet Oliveira, D.
Weygand, J.
Delano, K.
Zesta, E.
author_sort Oliveira, D.
title Superposed epoch analysis of ground dB/dt variations during shock-induced substorms: The role of shock inclination
title_short Superposed epoch analysis of ground dB/dt variations during shock-induced substorms: The role of shock inclination
title_full Superposed epoch analysis of ground dB/dt variations during shock-induced substorms: The role of shock inclination
title_fullStr Superposed epoch analysis of ground dB/dt variations during shock-induced substorms: The role of shock inclination
title_full_unstemmed Superposed epoch analysis of ground dB/dt variations during shock-induced substorms: The role of shock inclination
title_sort superposed epoch analysis of ground db/dt variations during shock-induced substorms: the role of shock inclination
publishDate 2023
url https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020489
geographic Greenland
geographic_facet Greenland
genre Greenland
Alaska
genre_facet Greenland
Alaska
op_source XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-3574
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020489
op_doi https://doi.org/10.57757/IUGG23-3574
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