Signature of 3600-yr LaViolette flare in Antarctica 10Be spectra

10Be deposition rates from Vostok, Antarctica raw ice core records are periodic with 3592±57 yr at 99% significance, verified against the 10Be concentration raw data from both Vostok, as 3700±57 yr at 99%, and Taylor Dome, Antarctica, as 3800±61 yr at 99%. Also, Mg concentration data from Taylor Dom...

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Main Author: Omerbashich, M.
Format: Report
Language:English
Published: 2021
Subjects:
Online Access:https://zenodo.org/record/5228497
https://doi.org/10.5281/zenodo.5228497
id ftzenodo:oai:zenodo.org:5228497
record_format openpolar
spelling ftzenodo:oai:zenodo.org:5228497 2023-05-15T13:42:46+02:00 Signature of 3600-yr LaViolette flare in Antarctica 10Be spectra Omerbashich, M. 2021-08-20 https://zenodo.org/record/5228497 https://doi.org/10.5281/zenodo.5228497 eng eng doi:10.5281/zenodo.5228496 https://zenodo.org/record/5228497 https://doi.org/10.5281/zenodo.5228497 oai:zenodo.org:5228497 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode Beryllium analysis Vostok ice cores cosmic rays paleoclimate Hallstadzeit cycle LaViolette flares High energy astrophysics Gamma-ray bursts Rapid bursts Supernovae Gamma-ray sources Gamma-ray transient sources Soft gamma-ray repeaters Galactic center Milky Way Galaxy physics Magnetars Milky Way magnetic fields Sky surveys Surface ices Cosmochemistry Cosmic abundances Chemical abundances Frozen-in elements Time series analysis Period search Gauss-Vaniček spectral analysis info:eu-repo/semantics/preprint publication-preprint 2021 ftzenodo https://doi.org/10.5281/zenodo.522849710.5281/zenodo.5228496 2023-03-11T00:40:58Z 10Be deposition rates from Vostok, Antarctica raw ice core records are periodic with 3592±57 yr at 99% significance, verified against the 10Be concentration raw data from both Vostok, as 3700±57 yr at 99%, and Taylor Dome, Antarctica, as 3800±61 yr at 99%. Also, Mg concentration data from Taylor Dome cycle every 3965±16 yr at 99%. The Vostok data respond to the Hallstadzeit Solar cycle, as 2296±57 yr at 99%, perhaps its best estimate yet. After data separation at 2·105 atoms/cm2/yr (deposition rates) and 0.95·105 atoms/g of ice (concentrations) cutoffs, reflecting cosmic-ray background conditions at the Galactic boundary, only the discovered period remains and converges, as 3378±103 yr and 3346±85 yr, respectively; the Hallstadzeit cycle vanishes in both cases. Thus the observed ~3600-yr period is of extrasolar but galactic origin. Since 10Be periodicity is explainable only by rapid excesses in the atmospheric cosmic-ray influx, the discovered period is the signature of a regular burst occurrence from a galactic source. Based on 500-parsec Galactic Center (GC) GeV/TeV γ-ray surveys by the H.E.S.S. and INTEGRAL telescopes, the GC’s extremely active central region makes the best candidate-host for such bursts recently observed by ROSAT and Fermi satellites. I estimate the most recent epoch of 10Be maximum as 1085±57 CE, coinciding with the 1054–1056 CE historical account apparently of SN1054 (Crab supernova), and predict the next maximum 10Be in 4463±57 CE. Given continuous decadeslong exposure and the relatively short return period coinciding with known cataclysms, this recurrent LaViolette flare affects the Earth climate significantly. Report Antarc* Antarctica ice core Zenodo Milky Way ENVELOPE(-68.705,-68.705,-71.251,-71.251) Taylor Dome ENVELOPE(157.667,157.667,-77.667,-77.667)
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language English
topic Beryllium analysis
Vostok ice cores
cosmic rays
paleoclimate
Hallstadzeit cycle
LaViolette flares
High energy astrophysics
Gamma-ray bursts
Rapid bursts
Supernovae
Gamma-ray sources
Gamma-ray transient sources
Soft gamma-ray repeaters
Galactic center
Milky Way Galaxy physics
Magnetars
Milky Way magnetic fields
Sky surveys
Surface ices
Cosmochemistry
Cosmic abundances
Chemical abundances
Frozen-in elements
Time series analysis
Period search
Gauss-Vaniček spectral analysis
spellingShingle Beryllium analysis
Vostok ice cores
cosmic rays
paleoclimate
Hallstadzeit cycle
LaViolette flares
High energy astrophysics
Gamma-ray bursts
Rapid bursts
Supernovae
Gamma-ray sources
Gamma-ray transient sources
Soft gamma-ray repeaters
Galactic center
Milky Way Galaxy physics
Magnetars
Milky Way magnetic fields
Sky surveys
Surface ices
Cosmochemistry
Cosmic abundances
Chemical abundances
Frozen-in elements
Time series analysis
Period search
Gauss-Vaniček spectral analysis
Omerbashich, M.
Signature of 3600-yr LaViolette flare in Antarctica 10Be spectra
topic_facet Beryllium analysis
Vostok ice cores
cosmic rays
paleoclimate
Hallstadzeit cycle
LaViolette flares
High energy astrophysics
Gamma-ray bursts
Rapid bursts
Supernovae
Gamma-ray sources
Gamma-ray transient sources
Soft gamma-ray repeaters
Galactic center
Milky Way Galaxy physics
Magnetars
Milky Way magnetic fields
Sky surveys
Surface ices
Cosmochemistry
Cosmic abundances
Chemical abundances
Frozen-in elements
Time series analysis
Period search
Gauss-Vaniček spectral analysis
description 10Be deposition rates from Vostok, Antarctica raw ice core records are periodic with 3592±57 yr at 99% significance, verified against the 10Be concentration raw data from both Vostok, as 3700±57 yr at 99%, and Taylor Dome, Antarctica, as 3800±61 yr at 99%. Also, Mg concentration data from Taylor Dome cycle every 3965±16 yr at 99%. The Vostok data respond to the Hallstadzeit Solar cycle, as 2296±57 yr at 99%, perhaps its best estimate yet. After data separation at 2·105 atoms/cm2/yr (deposition rates) and 0.95·105 atoms/g of ice (concentrations) cutoffs, reflecting cosmic-ray background conditions at the Galactic boundary, only the discovered period remains and converges, as 3378±103 yr and 3346±85 yr, respectively; the Hallstadzeit cycle vanishes in both cases. Thus the observed ~3600-yr period is of extrasolar but galactic origin. Since 10Be periodicity is explainable only by rapid excesses in the atmospheric cosmic-ray influx, the discovered period is the signature of a regular burst occurrence from a galactic source. Based on 500-parsec Galactic Center (GC) GeV/TeV γ-ray surveys by the H.E.S.S. and INTEGRAL telescopes, the GC’s extremely active central region makes the best candidate-host for such bursts recently observed by ROSAT and Fermi satellites. I estimate the most recent epoch of 10Be maximum as 1085±57 CE, coinciding with the 1054–1056 CE historical account apparently of SN1054 (Crab supernova), and predict the next maximum 10Be in 4463±57 CE. Given continuous decadeslong exposure and the relatively short return period coinciding with known cataclysms, this recurrent LaViolette flare affects the Earth climate significantly.
format Report
author Omerbashich, M.
author_facet Omerbashich, M.
author_sort Omerbashich, M.
title Signature of 3600-yr LaViolette flare in Antarctica 10Be spectra
title_short Signature of 3600-yr LaViolette flare in Antarctica 10Be spectra
title_full Signature of 3600-yr LaViolette flare in Antarctica 10Be spectra
title_fullStr Signature of 3600-yr LaViolette flare in Antarctica 10Be spectra
title_full_unstemmed Signature of 3600-yr LaViolette flare in Antarctica 10Be spectra
title_sort signature of 3600-yr laviolette flare in antarctica 10be spectra
publishDate 2021
url https://zenodo.org/record/5228497
https://doi.org/10.5281/zenodo.5228497
long_lat ENVELOPE(-68.705,-68.705,-71.251,-71.251)
ENVELOPE(157.667,157.667,-77.667,-77.667)
geographic Milky Way
Taylor Dome
geographic_facet Milky Way
Taylor Dome
genre Antarc*
Antarctica
ice core
genre_facet Antarc*
Antarctica
ice core
op_relation doi:10.5281/zenodo.5228496
https://zenodo.org/record/5228497
https://doi.org/10.5281/zenodo.5228497
oai:zenodo.org:5228497
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.522849710.5281/zenodo.5228496
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