Resumo

The earlier proposed hypothesis (Zuev et al., 2014) about the possibility of nanodispersed black carbon particles formation in eruptive column of volcanic eruption with VEI ³ 4 is discussed. The probable characteristics of volcanogenic soot particles and their distinctive features from stratospheric black carbon particles of other origin are analyzed. A brief review of suitable instrumental methods for detecting particles is carried out, and observational facts that indicate the possible detection of particles of volcanic soot earlier are presented. The idea of a complex experiment for observational confirmation of the hypothesis is proposed.
Título traduzido da contribuiçãoTHE HYPOTHESIS OF VOLCANOGENIC SOOT AND OPPORTUNITIES OF ITS OBSERVATIONAL CONFIRMATION
Idioma originalRussian
Páginas (de-até)463-470
Número de páginas8
RevistaОптика атмосферы и океана
Volume33
Número de emissão6 (377)
DOIs
Estado da publicaçãoPublished - 2020

GRNTI

  • 37.00.00 GEOPHYSICS

Level of Research Output

  • VAK List

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