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Stratospheric aerosol size reduction after volcanic eruptions

Stratospheric aerosol size reduction after volcanic eruptions

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_6e8dd684ca1747f09dea9ee64fd6d9c7

Stratospheric aerosol size reduction after volcanic eruptions

About this item

Full title

Stratospheric aerosol size reduction after volcanic eruptions

Publisher

Katlenburg-Lindau: Copernicus GmbH

Journal title

Atmospheric chemistry and physics, 2023-09, Vol.23 (17), p.9725-9743

Language

English

Formats

Publication information

Publisher

Katlenburg-Lindau: Copernicus GmbH

More information

Scope and Contents

Contents

The stratospheric aerosol layer plays an important role in the radiative balance of Earth primarily through scattering of solar radiation. The magnitude of this effect depends critically on the size distribution of the aerosol. The aerosol layer is in large part fed by volcanic eruptions strong enough to inject gaseous sulfur species into the strat...

Alternative Titles

Full title

Stratospheric aerosol size reduction after volcanic eruptions

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_doaj_primary_oai_doaj_org_article_6e8dd684ca1747f09dea9ee64fd6d9c7

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_6e8dd684ca1747f09dea9ee64fd6d9c7

Other Identifiers

ISSN

1680-7324,1680-7316

E-ISSN

1680-7324

DOI

10.5194/acp-23-9725-2023

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