A volcanism dependent model for the extinction profile of stratospheric aerosols in the UV-visible range

Details A volcanism dependent model for the extinction profile of stratospheric aerosols in the UV-visible range A volcanism dependent model for the extinction profile of stratospheric aerosols in the UV-visible range

Mar 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999georl..26..703f&link_type=abstract

Geophysical Research Letters, Volume 26, Issue 6, p. 703-706

Mathematics

Logic

8

Atmospheric Composition And Structure: Aerosols And Particles, Atmospheric Composition And Structure: Volcanic Effects

Scientific paper

We present a climatological model of the extinction coefficient of stratospheric aerosols in the UV-visible range based on SAGE II data. The model is a function of wavelength, latitude, relative altitude with respect to the tropopause and depends on the volcanism level. The vertical structure describes the tropopause region, the Junge layer and the high altitude domain. The model is shown to predict realistic extinction profiles with an reasonable accuracy.

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