Comment on "Atmospheric ionization by high-fluence, hard spectrum solar proton events and their probable appearance in the ice core archive" by A.L. Melott et al

Melott et al. [2016] suggest that individual solar proton events (SPEs) are detectable as nitrate ion spikes in ice cores. They use the high fluence, high energy (hard spectrum) SPE of 23 February 1956 to calculate an enhancement of HNO3 from the surface to 46 km that is equivalent to a ~120 ng cm-2...

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Main Authors: Duderstadt, K. A., Dibb, J. E., Jackman, C. H., Randall, C. E., Schwadron, N. A., Solomon, S. C., Spence, H. E.
Format: Text
Language:unknown
Published: arXiv 2016
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Online Access:https://dx.doi.org/10.48550/arxiv.1606.07471
https://arxiv.org/abs/1606.07471
id ftdatacite:10.48550/arxiv.1606.07471
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spelling ftdatacite:10.48550/arxiv.1606.07471 2023-05-15T16:38:45+02:00 Comment on "Atmospheric ionization by high-fluence, hard spectrum solar proton events and their probable appearance in the ice core archive" by A.L. Melott et al Duderstadt, K. A. Dibb, J. E. Jackman, C. H. Randall, C. E. Schwadron, N. A. Solomon, S. C. Spence, H. E. 2016 https://dx.doi.org/10.48550/arxiv.1606.07471 https://arxiv.org/abs/1606.07471 unknown arXiv https://dx.doi.org/10.1002/2016jd025220 arXiv.org perpetual, non-exclusive license http://arxiv.org/licenses/nonexclusive-distrib/1.0/ Atmospheric and Oceanic Physics physics.ao-ph Earth and Planetary Astrophysics astro-ph.EP Instrumentation and Methods for Astrophysics astro-ph.IM Solar and Stellar Astrophysics astro-ph.SR Geophysics physics.geo-ph FOS Physical sciences article-journal Article ScholarlyArticle Text 2016 ftdatacite https://doi.org/10.48550/arxiv.1606.07471 https://doi.org/10.1002/2016jd025220 2022-04-01T11:15:15Z Melott et al. [2016] suggest that individual solar proton events (SPEs) are detectable as nitrate ion spikes in ice cores. They use the high fluence, high energy (hard spectrum) SPE of 23 February 1956 to calculate an enhancement of HNO3 from the surface to 46 km that is equivalent to a ~120 ng cm-2 nitrate ion spike observed in the GISP2H ice core. The Melott et al. [2016] approach is fundamentally flawed, since it considers only the absolute column burden of SPE-produced nitrate and not the pre-existing nitrate in the stratosphere. Modeling studies supported by extensive observations [Duderstadt et al., 2014, 2016, and this comment] show background HNO3 in the lower and middle stratosphere equivalent to 2000 to 3000 ng cm-2 nitrate. These high levels of background nitrate must also be included when estimating SPE enhancements to the deposition of nitrate ions that might eventually be preserved in an ice core. The 1956 SPE results in less than a 5% increase in the column burden of atmospheric HNO3, not large enough to explain the nitrate spike seen in the GISP2H ice core. Even extreme SPE enhancements cannot explain nitrate peaks (typically hundreds of percent increases) observed in the ice record [Duderstadt et al., 2016]. Realistic mechanisms linking nitrate ions in ice cores to SPEs have not been established. It is time to move the search for indicators of SPEs away from nitrate ions: Nitrate ions cannot be used as proxies for individual SPEs in the ice core record. : 17 pages, 3 figures Corrected to address typographical error Text ice core DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Atmospheric and Oceanic Physics physics.ao-ph
Earth and Planetary Astrophysics astro-ph.EP
Instrumentation and Methods for Astrophysics astro-ph.IM
Solar and Stellar Astrophysics astro-ph.SR
Geophysics physics.geo-ph
FOS Physical sciences
spellingShingle Atmospheric and Oceanic Physics physics.ao-ph
Earth and Planetary Astrophysics astro-ph.EP
Instrumentation and Methods for Astrophysics astro-ph.IM
Solar and Stellar Astrophysics astro-ph.SR
Geophysics physics.geo-ph
FOS Physical sciences
Duderstadt, K. A.
Dibb, J. E.
Jackman, C. H.
Randall, C. E.
Schwadron, N. A.
Solomon, S. C.
Spence, H. E.
Comment on "Atmospheric ionization by high-fluence, hard spectrum solar proton events and their probable appearance in the ice core archive" by A.L. Melott et al
topic_facet Atmospheric and Oceanic Physics physics.ao-ph
Earth and Planetary Astrophysics astro-ph.EP
Instrumentation and Methods for Astrophysics astro-ph.IM
Solar and Stellar Astrophysics astro-ph.SR
Geophysics physics.geo-ph
FOS Physical sciences
description Melott et al. [2016] suggest that individual solar proton events (SPEs) are detectable as nitrate ion spikes in ice cores. They use the high fluence, high energy (hard spectrum) SPE of 23 February 1956 to calculate an enhancement of HNO3 from the surface to 46 km that is equivalent to a ~120 ng cm-2 nitrate ion spike observed in the GISP2H ice core. The Melott et al. [2016] approach is fundamentally flawed, since it considers only the absolute column burden of SPE-produced nitrate and not the pre-existing nitrate in the stratosphere. Modeling studies supported by extensive observations [Duderstadt et al., 2014, 2016, and this comment] show background HNO3 in the lower and middle stratosphere equivalent to 2000 to 3000 ng cm-2 nitrate. These high levels of background nitrate must also be included when estimating SPE enhancements to the deposition of nitrate ions that might eventually be preserved in an ice core. The 1956 SPE results in less than a 5% increase in the column burden of atmospheric HNO3, not large enough to explain the nitrate spike seen in the GISP2H ice core. Even extreme SPE enhancements cannot explain nitrate peaks (typically hundreds of percent increases) observed in the ice record [Duderstadt et al., 2016]. Realistic mechanisms linking nitrate ions in ice cores to SPEs have not been established. It is time to move the search for indicators of SPEs away from nitrate ions: Nitrate ions cannot be used as proxies for individual SPEs in the ice core record. : 17 pages, 3 figures Corrected to address typographical error
format Text
author Duderstadt, K. A.
Dibb, J. E.
Jackman, C. H.
Randall, C. E.
Schwadron, N. A.
Solomon, S. C.
Spence, H. E.
author_facet Duderstadt, K. A.
Dibb, J. E.
Jackman, C. H.
Randall, C. E.
Schwadron, N. A.
Solomon, S. C.
Spence, H. E.
author_sort Duderstadt, K. A.
title Comment on "Atmospheric ionization by high-fluence, hard spectrum solar proton events and their probable appearance in the ice core archive" by A.L. Melott et al
title_short Comment on "Atmospheric ionization by high-fluence, hard spectrum solar proton events and their probable appearance in the ice core archive" by A.L. Melott et al
title_full Comment on "Atmospheric ionization by high-fluence, hard spectrum solar proton events and their probable appearance in the ice core archive" by A.L. Melott et al
title_fullStr Comment on "Atmospheric ionization by high-fluence, hard spectrum solar proton events and their probable appearance in the ice core archive" by A.L. Melott et al
title_full_unstemmed Comment on "Atmospheric ionization by high-fluence, hard spectrum solar proton events and their probable appearance in the ice core archive" by A.L. Melott et al
title_sort comment on "atmospheric ionization by high-fluence, hard spectrum solar proton events and their probable appearance in the ice core archive" by a.l. melott et al
publisher arXiv
publishDate 2016
url https://dx.doi.org/10.48550/arxiv.1606.07471
https://arxiv.org/abs/1606.07471
genre ice core
genre_facet ice core
op_relation https://dx.doi.org/10.1002/2016jd025220
op_rights arXiv.org perpetual, non-exclusive license
http://arxiv.org/licenses/nonexclusive-distrib/1.0/
op_doi https://doi.org/10.48550/arxiv.1606.07471
https://doi.org/10.1002/2016jd025220
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