2020
DOI: 10.3847/1538-4357/aba1f2
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Connecting 3D Evolution of Coronal Mass Ejections to Their Source Regions

Abstract: Since Coronal Mass Ejections (CMEs) are the major drivers of space weather, it is crucial to study their evolution starting from the inner corona. In this work we use Graduated Cylindrical Shell (GCS) model to study the 3D evolution of 59 CMEs in the inner (< 3R ) and outer (> 3R ) corona using observations from COR-1 and COR-2 on-board Solar TErrestrial RElations Observatory (STEREO) spacecraft. We identify the source regions of these CMEs and classify them as CMEs associated with Active Regions (ARs), Active… Show more

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Cited by 26 publications
(74 citation statements)
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“…For this we included a total of 1,064 events that occurred during 2000-2002, 2008, 2009, and also from 2012 to 2014, which covers the maxima of cycle 23, the minima of cycle 24 and the maxima of cycle 24. Here, we have followed a similar method as reported in Majumdar et al (2020) and using the JHelioviewer software (Muller et al, 2009;Müller et al, 2017) to back-project the CMEs onto the solar disk. We further segregated the identified source regions of the CMEs into two broad categories, namely 1) Active Regions(ARs) and 2) Prominence Eruptions(PEs).…”
Section: Segregation Of the Slow And Fast Cmes On The Basis Of Their Source Regionmentioning
confidence: 99%
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“…For this we included a total of 1,064 events that occurred during 2000-2002, 2008, 2009, and also from 2012 to 2014, which covers the maxima of cycle 23, the minima of cycle 24 and the maxima of cycle 24. Here, we have followed a similar method as reported in Majumdar et al (2020) and using the JHelioviewer software (Muller et al, 2009;Müller et al, 2017) to back-project the CMEs onto the solar disk. We further segregated the identified source regions of the CMEs into two broad categories, namely 1) Active Regions(ARs) and 2) Prominence Eruptions(PEs).…”
Section: Segregation Of the Slow And Fast Cmes On The Basis Of Their Source Regionmentioning
confidence: 99%
“…For a spatial association (see Gilbert et al, 2000;Majumdar et al, 2020) between a source region and a subsequent CME, we require that the latitude of the source region to be around ± 30°t o that of the PA of the center of the CME as reported in the CDAW catalog. In the case of a filament eruption, due to larger uncertainty of its spatial location, we look for an erupting filament around ± 40°around the PA of the CME converted to equivalent apparent latitude (lat PA ) by the following relation:…”
Section: Segregation Of the Slow And Fast Cmes On The Basis Of Their Source Regionmentioning
confidence: 99%
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