Dayside Magnetic Depression Following Interplanetary Shock Arrivals During the February 1958 and July 1959 Superstorms

Abstract The present study investigates mid‐ and low‐latitude ground magnetic disturbances observed following the arrival of three interplanetary (IP) shocks during the super‐geomagnetic storms of February 1958 and July 1959. One may expect that after IP shocks, the H (northward) magnetic component...

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Main Authors: Shinichi Ohtani, Yoko Odagi, Ayako Matsuoka, Toshihiko Iyemori
Format: Article
Language:English
Published: Wiley 2024-10-01
Series:Space Weather
Subjects:
Online Access:https://doi.org/10.1029/2024SW004017
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author Shinichi Ohtani
Yoko Odagi
Ayako Matsuoka
Toshihiko Iyemori
author_facet Shinichi Ohtani
Yoko Odagi
Ayako Matsuoka
Toshihiko Iyemori
author_sort Shinichi Ohtani
collection DOAJ
description Abstract The present study investigates mid‐ and low‐latitude ground magnetic disturbances observed following the arrival of three interplanetary (IP) shocks during the super‐geomagnetic storms of February 1958 and July 1959. One may expect that after IP shocks, the H (northward) magnetic component increases globally but especially on the dayside. However, in each event, the H component was depressed sharply for 1–2 hr in the dawn‐to‐noon sector, whereas it increased in other local time (LT) sectors. Observed magnetic deflections suggest that there existed field‐aligned currents (FACs) flowing into and out of the auroral zone around the western and eastern edges of the LT sector of the dayside H depression. These features strongly suggests that the observed H depression was a remote effect of a R1‐sense FAC system. It was previously reported that similar ground magnetic disturbances were observed after the SSC of the 2003 Halloween storm, which reveals striking similarities to the well‐known H depression observed at Colaba during the 1859 Carrington storm. It is therefore suggested that the external driving behind IP shocks, especially those associated with major storms, is most optimum for the sharp reduction of the dayside H component through the formation and intensification of the dayside FAC system. Associated magnetic disturbances are considered to be larger in magnitude with increasing magnetic latitude, and oriented azimuthally as well as meridionally. Such magnetic disturbances in dayside midlatitudes may not be discussed very often as a target of space weather, but their potential impacts on ground infrastructures probably require closer attention.
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spelling doaj-art-e2900e38fb1144689517ad2946a1bf822025-01-14T16:31:08ZengWileySpace Weather1542-73902024-10-012210n/an/a10.1029/2024SW004017Dayside Magnetic Depression Following Interplanetary Shock Arrivals During the February 1958 and July 1959 SuperstormsShinichi Ohtani0Yoko Odagi1Ayako Matsuoka2Toshihiko Iyemori3Johns Hopkins University Applied Physics Laboratory Laurel MD USAData Analysis Center for Geomagnetism and Space Magnetism Graduate School of Science Kyoto University Kyoto JapanData Analysis Center for Geomagnetism and Space Magnetism Graduate School of Science Kyoto University Kyoto JapanData Analysis Center for Geomagnetism and Space Magnetism Graduate School of Science Kyoto University Kyoto JapanAbstract The present study investigates mid‐ and low‐latitude ground magnetic disturbances observed following the arrival of three interplanetary (IP) shocks during the super‐geomagnetic storms of February 1958 and July 1959. One may expect that after IP shocks, the H (northward) magnetic component increases globally but especially on the dayside. However, in each event, the H component was depressed sharply for 1–2 hr in the dawn‐to‐noon sector, whereas it increased in other local time (LT) sectors. Observed magnetic deflections suggest that there existed field‐aligned currents (FACs) flowing into and out of the auroral zone around the western and eastern edges of the LT sector of the dayside H depression. These features strongly suggests that the observed H depression was a remote effect of a R1‐sense FAC system. It was previously reported that similar ground magnetic disturbances were observed after the SSC of the 2003 Halloween storm, which reveals striking similarities to the well‐known H depression observed at Colaba during the 1859 Carrington storm. It is therefore suggested that the external driving behind IP shocks, especially those associated with major storms, is most optimum for the sharp reduction of the dayside H component through the formation and intensification of the dayside FAC system. Associated magnetic disturbances are considered to be larger in magnitude with increasing magnetic latitude, and oriented azimuthally as well as meridionally. Such magnetic disturbances in dayside midlatitudes may not be discussed very often as a target of space weather, but their potential impacts on ground infrastructures probably require closer attention.https://doi.org/10.1029/2024SW004017superstormsdayside geomagnetic depressionstorm sudden commencementdayside current wedgesolar wind compressionsolar wind‐magnetosphere‐ionosphere coupling
spellingShingle Shinichi Ohtani
Yoko Odagi
Ayako Matsuoka
Toshihiko Iyemori
Dayside Magnetic Depression Following Interplanetary Shock Arrivals During the February 1958 and July 1959 Superstorms
Space Weather
superstorms
dayside geomagnetic depression
storm sudden commencement
dayside current wedge
solar wind compression
solar wind‐magnetosphere‐ionosphere coupling
title Dayside Magnetic Depression Following Interplanetary Shock Arrivals During the February 1958 and July 1959 Superstorms
title_full Dayside Magnetic Depression Following Interplanetary Shock Arrivals During the February 1958 and July 1959 Superstorms
title_fullStr Dayside Magnetic Depression Following Interplanetary Shock Arrivals During the February 1958 and July 1959 Superstorms
title_full_unstemmed Dayside Magnetic Depression Following Interplanetary Shock Arrivals During the February 1958 and July 1959 Superstorms
title_short Dayside Magnetic Depression Following Interplanetary Shock Arrivals During the February 1958 and July 1959 Superstorms
title_sort dayside magnetic depression following interplanetary shock arrivals during the february 1958 and july 1959 superstorms
topic superstorms
dayside geomagnetic depression
storm sudden commencement
dayside current wedge
solar wind compression
solar wind‐magnetosphere‐ionosphere coupling
url https://doi.org/10.1029/2024SW004017
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AT ayakomatsuoka daysidemagneticdepressionfollowinginterplanetaryshockarrivalsduringthefebruary1958andjuly1959superstorms
AT toshihikoiyemori daysidemagneticdepressionfollowinginterplanetaryshockarrivalsduringthefebruary1958andjuly1959superstorms