Terrestrial impact of the galactic historical SNeстатья
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Дата последнего поиска статьи во внешних источниках: 18 июля 2013 г.
Аннотация:Galactic supernovae (SNe) of the last millennium have left their signatures in many energy domains, with the optical being the best known due to the absence of astronomical instruments before the 17th century being more sophisticated than the human eye. Alongside with these records found in the scriptes of the ancient eastern and western astronomers, quite recently other signatures were recognised as valuable tracers of historical SNe, for example, different ionic and/or molecular depositions in the polar ice, radioactive isotopes depositions, and the /γ-ray emission from the radioactive 44Ti produced in the SN explosion. While the ice depositions are expected to be the result of the supernova flash in the UV and soft X-rays, the 60Fe radioactive isotope deposition into the deep-ocean ferromanganese crust is the result of direct isotope transfer by cosmic rays dust grains originating in the SN blast wave. These and other impacts of the galactic SNe are important from the point of view of their possible influence on the terrestrial environment. In this paper we consider known tracers of historical SNe and compare them to the proposed new tracer based on the atmospheric response to the galactic supernova emission in the UV and X-rays. In addition to using the 44Ti radioactive decay line photons for uncovering hidden galactic supernova remnants by imaging /γ-ray telescopes, all such tracers form an important complement to the historical SNe record.