Fate of volcanic ash: Aggregation and fallout | Zendy

William I. Rose | Zendy; A. J. Durant | Zendy

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Fate of volcanic ash: Aggregation and fallout

Author(s) -

William I. Rose,

A. J. Durant

Publication year - 2011

Publication title -

geology

Language(s) - English

Resource type - Journals

SCImago Journal Rank - 2.609

H-Index - 215

eISSN - 1943-2682

pISSN - 0091-7613

DOI - 10.1130/focus092011.1

Subject(s) - volcanic ash , volcano , atmosphere (unit) , atmospheric sciences , sulfate , radiative transfer , aerosol , geology , stratosphere , environmental science , earth science , residence time (fluid dynamics) , sulfate aerosol , vulcanian eruption , climatology , geochemistry , meteorology , chemistry , geography , geotechnical engineering , physics , organic chemistry , quantum mechanics

While suspended in Earth's atmosphere, fine ash influences radiative transfer, weather, and climate (e.g., [Newhall and Self, 1982][1]). Sulfate aerosol, also in volcanic ash clouds, dominates atmospheric effects, having stratospheric residence times of months to years ([Robock, 2000][2]), so large

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