Effects of Geometries and Substructures of ICMEs on Geomagnetic Storms

To better understand geomagnetic storm generations by ICMEs, we consider the effect of substructures (magnetic cloud, MC, and sheath) and geometries (impact location of flux-rope at the Earth) of the ICMEs. We apply the toroidal magnetic flux-rope model to 59 CDAW CME–ICME pairs to identify their su...

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Veröffentlicht in:Solar physics 2018-09, Vol.293 (9), p.1-20, Article 129
Hauptverfasser: Lee, Jae-Ok, Cho, Kyung-Suk, Kim, Rok-Soon, Jang, Soojeong, Marubashi, Katsuhide
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container_issue 9
container_start_page 1
container_title Solar physics
container_volume 293
creator Lee, Jae-Ok
Cho, Kyung-Suk
Kim, Rok-Soon
Jang, Soojeong
Marubashi, Katsuhide
description To better understand geomagnetic storm generations by ICMEs, we consider the effect of substructures (magnetic cloud, MC, and sheath) and geometries (impact location of flux-rope at the Earth) of the ICMEs. We apply the toroidal magnetic flux-rope model to 59 CDAW CME–ICME pairs to identify their substructures and geometries, and select 20 MC-associated and five sheath-associated storm events. We investigate the relationship between the storm strength indicated by minimum Dst index ( Dst min ) and solar wind conditions related to a southward magnetic field. We find that all slopes of linear regression lines for sheath-storm events are steeper ( ≥ 1.4 ) than those of the MC-storm events in the relationship between Dst min and solar wind conditions, implying that the efficiency of sheath for the process of geomagnetic storm generations is higher than that of MC. These results suggest that different general solar wind conditions (sheaths have a higher density, dynamic and thermal pressures with a higher fluctuation of the parameters and higher magnetic fields than MCs) have different impact on storm generation. Regarding the geometric encounter of ICMEs, 100% (2/2) of major storms ( Dst min ≤ − 100 nT ) occur in the regions at negative  P Y (relative position of the Earth trajectory from the ICME axis in the Y component of the GSE coordinate) when the eastern flanks of ICMEs encounter the Earth. We find similar statistical trends in solar wind conditions, suggesting that the dependence of geomagnetic storms on 3D ICME–Earth impact geometries is caused by asymmetric distributions of the geoeffective solar wind conditions. For western flank events, 80% (4/5) of the major storms occur in positive P Y regions, while intense geoeffective solar wind conditions are not located in the positive P Y . These results suggest that the strength of geomagnetic storms depends on ICME–Earth impact geometries as they determine the solar wind conditions at Earth.
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Regarding the geometric encounter of ICMEs, 100% (2/2) of major storms ( Dst min ≤ − 100 nT ) occur in the regions at negative  P Y (relative position of the Earth trajectory from the ICME axis in the Y component of the GSE coordinate) when the eastern flanks of ICMEs encounter the Earth. We find similar statistical trends in solar wind conditions, suggesting that the dependence of geomagnetic storms on 3D ICME–Earth impact geometries is caused by asymmetric distributions of the geoeffective solar wind conditions. For western flank events, 80% (4/5) of the major storms occur in positive P Y regions, while intense geoeffective solar wind conditions are not located in the positive P Y . 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subjects Astrophysics and Astroparticles
Atmospheric Sciences
Dependence
DST Index
Earth
Geomagnetic storms
Geomagnetism
Magnetic clouds
Magnetic fields
Magnetic flux
Magnetic storms
Physics
Physics and Astronomy
Saturn
Sheaths
Skewed distributions
Solar physics
Solar wind
Space Exploration and Astronautics
Space Sciences (including Extraterrestrial Physics
Statistical analysis
Storms
Substructures
Variation
title Effects of Geometries and Substructures of ICMEs on Geomagnetic Storms
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