author_facet Li, G.
Zank, G. P.
Li, G.
Zank, G. P.
author Li, G.
Zank, G. P.
spellingShingle Li, G.
Zank, G. P.
Geophysical Research Letters
Mixed particle acceleration at CME‐driven shocks and flares
General Earth and Planetary Sciences
Geophysics
author_sort li, g.
spelling Li, G. Zank, G. P. 0094-8276 1944-8007 American Geophysical Union (AGU) General Earth and Planetary Sciences Geophysics http://dx.doi.org/10.1029/2004gl021250 <jats:p>A recent study of <jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="#grl18983-bib-0003"><jats:italic>Cane et al.</jats:italic> [2003]</jats:ext-link> showed that in some intense SEP events, the time‐intensity profiles exhibit two peaks, with an earlier one having a high <jats:italic>Fe</jats:italic>/<jats:italic>O</jats:italic> and a later one with a low <jats:italic>Fe</jats:italic>/<jats:italic>O</jats:italic> ratio. They suggested that these two‐component events are due to CMEs and their accompanying flares occurring together, with the first peak being flare‐related and the second peak being CME‐driven shock related. In this paper, we develop a model which examines particle acceleration and transport when both flares and CME‐driven shocks are present. We study time‐intensity profiles for three different scenarios: a pure shock case, a pure flare case and a shock‐flare‐mixed case. Using reasonable estimates of the relative timing between CMEs and associated flares, we find that a large portion of the flare accelerated material is subject to absorption and re‐acceleration by the CME‐driven shock. Consequently, the time intensity profile for the shock‐flare‐mixed case shows an initial rapid increase, owing to particles accelerated at the flare and followed by a plateau similar to that of a pure shock case.</jats:p> Mixed particle acceleration at CME‐driven shocks and flares Geophysical Research Letters
doi_str_mv 10.1029/2004gl021250
facet_avail Online
Free
finc_class_facet Geologie und Paläontologie
Geographie
Physik
format ElectronicArticle
fullrecord blob:ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTAyOS8yMDA0Z2wwMjEyNTA
id ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTAyOS8yMDA0Z2wwMjEyNTA
institution DE-Bn3
DE-Brt1
DE-Zwi2
DE-D161
DE-Gla1
DE-Zi4
DE-15
DE-Pl11
DE-Rs1
DE-105
DE-14
DE-Ch1
DE-L229
DE-D275
imprint American Geophysical Union (AGU), 2005
imprint_str_mv American Geophysical Union (AGU), 2005
issn 0094-8276
1944-8007
issn_str_mv 0094-8276
1944-8007
language English
mega_collection American Geophysical Union (AGU) (CrossRef)
match_str li2005mixedparticleaccelerationatcmedrivenshocksandflares
publishDateSort 2005
publisher American Geophysical Union (AGU)
recordtype ai
record_format ai
series Geophysical Research Letters
source_id 49
title Mixed particle acceleration at CME‐driven shocks and flares
title_unstemmed Mixed particle acceleration at CME‐driven shocks and flares
title_full Mixed particle acceleration at CME‐driven shocks and flares
title_fullStr Mixed particle acceleration at CME‐driven shocks and flares
title_full_unstemmed Mixed particle acceleration at CME‐driven shocks and flares
title_short Mixed particle acceleration at CME‐driven shocks and flares
title_sort mixed particle acceleration at cme‐driven shocks and flares
topic General Earth and Planetary Sciences
Geophysics
url http://dx.doi.org/10.1029/2004gl021250
publishDate 2005
physical
description <jats:p>A recent study of <jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="#grl18983-bib-0003"><jats:italic>Cane et al.</jats:italic> [2003]</jats:ext-link> showed that in some intense SEP events, the time‐intensity profiles exhibit two peaks, with an earlier one having a high <jats:italic>Fe</jats:italic>/<jats:italic>O</jats:italic> and a later one with a low <jats:italic>Fe</jats:italic>/<jats:italic>O</jats:italic> ratio. They suggested that these two‐component events are due to CMEs and their accompanying flares occurring together, with the first peak being flare‐related and the second peak being CME‐driven shock related. In this paper, we develop a model which examines particle acceleration and transport when both flares and CME‐driven shocks are present. We study time‐intensity profiles for three different scenarios: a pure shock case, a pure flare case and a shock‐flare‐mixed case. Using reasonable estimates of the relative timing between CMEs and associated flares, we find that a large portion of the flare accelerated material is subject to absorption and re‐acceleration by the CME‐driven shock. Consequently, the time intensity profile for the shock‐flare‐mixed case shows an initial rapid increase, owing to particles accelerated at the flare and followed by a plateau similar to that of a pure shock case.</jats:p>
container_issue 2
container_start_page 0
container_title Geophysical Research Letters
container_volume 32
format_de105 Article, E-Article
format_de14 Article, E-Article
format_de15 Article, E-Article
format_de520 Article, E-Article
format_de540 Article, E-Article
format_dech1 Article, E-Article
format_ded117 Article, E-Article
format_degla1 E-Article
format_del152 Buch
format_del189 Article, E-Article
format_dezi4 Article
format_dezwi2 Article, E-Article
format_finc Article, E-Article
format_nrw Article, E-Article
_version_ 1792342318108377099
geogr_code not assigned
last_indexed 2024-03-01T16:33:45.014Z
geogr_code_person not assigned
openURL url_ver=Z39.88-2004&ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fvufind.svn.sourceforge.net%3Agenerator&rft.title=Mixed+particle+acceleration+at+CME%E2%80%90driven+shocks+and+flares&rft.date=2005-01-01&genre=article&issn=1944-8007&volume=32&issue=2&jtitle=Geophysical+Research+Letters&atitle=Mixed+particle+acceleration+at+CME%E2%80%90driven+shocks+and+flares&aulast=Zank&aufirst=G.+P.&rft_id=info%3Adoi%2F10.1029%2F2004gl021250&rft.language%5B0%5D=eng
SOLR
_version_ 1792342318108377099
author Li, G., Zank, G. P.
author_facet Li, G., Zank, G. P., Li, G., Zank, G. P.
author_sort li, g.
container_issue 2
container_start_page 0
container_title Geophysical Research Letters
container_volume 32
description <jats:p>A recent study of <jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="#grl18983-bib-0003"><jats:italic>Cane et al.</jats:italic> [2003]</jats:ext-link> showed that in some intense SEP events, the time‐intensity profiles exhibit two peaks, with an earlier one having a high <jats:italic>Fe</jats:italic>/<jats:italic>O</jats:italic> and a later one with a low <jats:italic>Fe</jats:italic>/<jats:italic>O</jats:italic> ratio. They suggested that these two‐component events are due to CMEs and their accompanying flares occurring together, with the first peak being flare‐related and the second peak being CME‐driven shock related. In this paper, we develop a model which examines particle acceleration and transport when both flares and CME‐driven shocks are present. We study time‐intensity profiles for three different scenarios: a pure shock case, a pure flare case and a shock‐flare‐mixed case. Using reasonable estimates of the relative timing between CMEs and associated flares, we find that a large portion of the flare accelerated material is subject to absorption and re‐acceleration by the CME‐driven shock. Consequently, the time intensity profile for the shock‐flare‐mixed case shows an initial rapid increase, owing to particles accelerated at the flare and followed by a plateau similar to that of a pure shock case.</jats:p>
doi_str_mv 10.1029/2004gl021250
facet_avail Online, Free
finc_class_facet Geologie und Paläontologie, Geographie, Physik
format ElectronicArticle
format_de105 Article, E-Article
format_de14 Article, E-Article
format_de15 Article, E-Article
format_de520 Article, E-Article
format_de540 Article, E-Article
format_dech1 Article, E-Article
format_ded117 Article, E-Article
format_degla1 E-Article
format_del152 Buch
format_del189 Article, E-Article
format_dezi4 Article
format_dezwi2 Article, E-Article
format_finc Article, E-Article
format_nrw Article, E-Article
geogr_code not assigned
geogr_code_person not assigned
id ai-49-aHR0cDovL2R4LmRvaS5vcmcvMTAuMTAyOS8yMDA0Z2wwMjEyNTA
imprint American Geophysical Union (AGU), 2005
imprint_str_mv American Geophysical Union (AGU), 2005
institution DE-Bn3, DE-Brt1, DE-Zwi2, DE-D161, DE-Gla1, DE-Zi4, DE-15, DE-Pl11, DE-Rs1, DE-105, DE-14, DE-Ch1, DE-L229, DE-D275
issn 0094-8276, 1944-8007
issn_str_mv 0094-8276, 1944-8007
language English
last_indexed 2024-03-01T16:33:45.014Z
match_str li2005mixedparticleaccelerationatcmedrivenshocksandflares
mega_collection American Geophysical Union (AGU) (CrossRef)
physical
publishDate 2005
publishDateSort 2005
publisher American Geophysical Union (AGU)
record_format ai
recordtype ai
series Geophysical Research Letters
source_id 49
spelling Li, G. Zank, G. P. 0094-8276 1944-8007 American Geophysical Union (AGU) General Earth and Planetary Sciences Geophysics http://dx.doi.org/10.1029/2004gl021250 <jats:p>A recent study of <jats:ext-link xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="#grl18983-bib-0003"><jats:italic>Cane et al.</jats:italic> [2003]</jats:ext-link> showed that in some intense SEP events, the time‐intensity profiles exhibit two peaks, with an earlier one having a high <jats:italic>Fe</jats:italic>/<jats:italic>O</jats:italic> and a later one with a low <jats:italic>Fe</jats:italic>/<jats:italic>O</jats:italic> ratio. They suggested that these two‐component events are due to CMEs and their accompanying flares occurring together, with the first peak being flare‐related and the second peak being CME‐driven shock related. In this paper, we develop a model which examines particle acceleration and transport when both flares and CME‐driven shocks are present. We study time‐intensity profiles for three different scenarios: a pure shock case, a pure flare case and a shock‐flare‐mixed case. Using reasonable estimates of the relative timing between CMEs and associated flares, we find that a large portion of the flare accelerated material is subject to absorption and re‐acceleration by the CME‐driven shock. Consequently, the time intensity profile for the shock‐flare‐mixed case shows an initial rapid increase, owing to particles accelerated at the flare and followed by a plateau similar to that of a pure shock case.</jats:p> Mixed particle acceleration at CME‐driven shocks and flares Geophysical Research Letters
spellingShingle Li, G., Zank, G. P., Geophysical Research Letters, Mixed particle acceleration at CME‐driven shocks and flares, General Earth and Planetary Sciences, Geophysics
title Mixed particle acceleration at CME‐driven shocks and flares
title_full Mixed particle acceleration at CME‐driven shocks and flares
title_fullStr Mixed particle acceleration at CME‐driven shocks and flares
title_full_unstemmed Mixed particle acceleration at CME‐driven shocks and flares
title_short Mixed particle acceleration at CME‐driven shocks and flares
title_sort mixed particle acceleration at cme‐driven shocks and flares
title_unstemmed Mixed particle acceleration at CME‐driven shocks and flares
topic General Earth and Planetary Sciences, Geophysics
url http://dx.doi.org/10.1029/2004gl021250