Short- and medium-term atmospheric effects of very large solar proton events
International audience Solar eruptions sometimes produce protons, which impact the Earth's atmosphere. These solar proton events (SPEs) generally last a few days and produce high energy particles that precipitate into the Earth's atmosphere. The protons cause ionization and dissociation pr...
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ftinsu:oai:HAL:hal-00302989v1 2023-11-12T04:24:55+01:00 Short- and medium-term atmospheric effects of very large solar proton events Jackman, C. H. Marsh, D. R. Vitt, F. M. Garcia, R. R. Fleming, E. L. Labow, G. J. Randall, C. E. López-Puertas, M. Funke, B. NASA Goddard Space Flight Center (GSFC) National Center for Atmospheric Research Boulder (NCAR) University of Colorado Boulder Instituto de Astrofísica de Andalucía (IAA) Consejo Superior de Investigaciones Cientificas = Spanish National Research Council (CSIC) 2007-07-23 https://hal.science/hal-00302989 https://hal.science/hal-00302989/document https://hal.science/hal-00302989/file/acpd-7-10543-2007.pdf en eng HAL CCSD European Geosciences Union hal-00302989 https://hal.science/hal-00302989 https://hal.science/hal-00302989/document https://hal.science/hal-00302989/file/acpd-7-10543-2007.pdf info:eu-repo/semantics/OpenAccess ISSN: 1680-7367 EISSN: 1680-7375 Atmospheric Chemistry and Physics Discussions https://hal.science/hal-00302989 Atmospheric Chemistry and Physics Discussions, 2007, 7 (4), pp.10543-10588 [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere info:eu-repo/semantics/article Journal articles 2007 ftinsu 2023-10-25T16:26:26Z International audience Solar eruptions sometimes produce protons, which impact the Earth's atmosphere. These solar proton events (SPEs) generally last a few days and produce high energy particles that precipitate into the Earth's atmosphere. The protons cause ionization and dissociation processes that ultimately lead to an enhancement of odd-hydrogen and odd-nitrogen in the polar cap regions (>60° geomagnetic latitude). We have used the Whole Atmosphere Community Climate Model (WACCM3) to study the atmospheric impact of SPEs over the period 1963?2005. The very largest SPEs were found to be the most important and caused atmospheric effects that lasted several months to years after the events. We present the short- and medium-term (days to a few months) atmospheric influence of the four largest SPEs in the past 45 years (August 1972; October 1989; July 2000; and October?November 2003) as computed by WACCM3 and observed by satellite instruments. The polar effects can be summarized as follows: 1) Mesospheric NO x (NO+NO 2 ) increased by over 50 ppbv and mesospheric ozone decreased by over 30% during these very large SPEs; 2) upper stratospheric and lower mesospheric NO x increased by over 10 ppbv and was transported during polar night down to the middle stratosphere in a few weeks; 3) mid- to upper stratospheric ozone decreased over 20%; and 4) enhancements of HNO 3 , HOCl, ClO, ClONO 2 , and N 2 O 5 were indirectly caused by the very large SPEs, although the model results suggest impacts at higher altitudes than indicated by the measurements for the October?November 2003 SPE period. Article in Journal/Newspaper polar night Institut national des sciences de l'Univers: HAL-INSU |
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Open Polar |
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Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
ftinsu |
language |
English |
topic |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere |
spellingShingle |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere Jackman, C. H. Marsh, D. R. Vitt, F. M. Garcia, R. R. Fleming, E. L. Labow, G. J. Randall, C. E. López-Puertas, M. Funke, B. Short- and medium-term atmospheric effects of very large solar proton events |
topic_facet |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere |
description |
International audience Solar eruptions sometimes produce protons, which impact the Earth's atmosphere. These solar proton events (SPEs) generally last a few days and produce high energy particles that precipitate into the Earth's atmosphere. The protons cause ionization and dissociation processes that ultimately lead to an enhancement of odd-hydrogen and odd-nitrogen in the polar cap regions (>60° geomagnetic latitude). We have used the Whole Atmosphere Community Climate Model (WACCM3) to study the atmospheric impact of SPEs over the period 1963?2005. The very largest SPEs were found to be the most important and caused atmospheric effects that lasted several months to years after the events. We present the short- and medium-term (days to a few months) atmospheric influence of the four largest SPEs in the past 45 years (August 1972; October 1989; July 2000; and October?November 2003) as computed by WACCM3 and observed by satellite instruments. The polar effects can be summarized as follows: 1) Mesospheric NO x (NO+NO 2 ) increased by over 50 ppbv and mesospheric ozone decreased by over 30% during these very large SPEs; 2) upper stratospheric and lower mesospheric NO x increased by over 10 ppbv and was transported during polar night down to the middle stratosphere in a few weeks; 3) mid- to upper stratospheric ozone decreased over 20%; and 4) enhancements of HNO 3 , HOCl, ClO, ClONO 2 , and N 2 O 5 were indirectly caused by the very large SPEs, although the model results suggest impacts at higher altitudes than indicated by the measurements for the October?November 2003 SPE period. |
author2 |
NASA Goddard Space Flight Center (GSFC) National Center for Atmospheric Research Boulder (NCAR) University of Colorado Boulder Instituto de Astrofísica de Andalucía (IAA) Consejo Superior de Investigaciones Cientificas = Spanish National Research Council (CSIC) |
format |
Article in Journal/Newspaper |
author |
Jackman, C. H. Marsh, D. R. Vitt, F. M. Garcia, R. R. Fleming, E. L. Labow, G. J. Randall, C. E. López-Puertas, M. Funke, B. |
author_facet |
Jackman, C. H. Marsh, D. R. Vitt, F. M. Garcia, R. R. Fleming, E. L. Labow, G. J. Randall, C. E. López-Puertas, M. Funke, B. |
author_sort |
Jackman, C. H. |
title |
Short- and medium-term atmospheric effects of very large solar proton events |
title_short |
Short- and medium-term atmospheric effects of very large solar proton events |
title_full |
Short- and medium-term atmospheric effects of very large solar proton events |
title_fullStr |
Short- and medium-term atmospheric effects of very large solar proton events |
title_full_unstemmed |
Short- and medium-term atmospheric effects of very large solar proton events |
title_sort |
short- and medium-term atmospheric effects of very large solar proton events |
publisher |
HAL CCSD |
publishDate |
2007 |
url |
https://hal.science/hal-00302989 https://hal.science/hal-00302989/document https://hal.science/hal-00302989/file/acpd-7-10543-2007.pdf |
genre |
polar night |
genre_facet |
polar night |
op_source |
ISSN: 1680-7367 EISSN: 1680-7375 Atmospheric Chemistry and Physics Discussions https://hal.science/hal-00302989 Atmospheric Chemistry and Physics Discussions, 2007, 7 (4), pp.10543-10588 |
op_relation |
hal-00302989 https://hal.science/hal-00302989 https://hal.science/hal-00302989/document https://hal.science/hal-00302989/file/acpd-7-10543-2007.pdf |
op_rights |
info:eu-repo/semantics/OpenAccess |
_version_ |
1782339371872026624 |