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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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 |
_version_ |
1766172703876710400 |