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The effect of stratospheric sulfur from Mount Pinatubo on tropospheric oxidizing capacity and methane
Author(s) -
Bândă Narcisa,
Krol Maarten,
Noije Twan,
Weele Michiel,
Williams Jason E.,
Sager Philippe Le,
Niemeier Ulrike,
Thomason Larry,
Röckmann Thomas
Publication year - 2015
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1002/2014jd022137
Subject(s) - troposphere , stratosphere , atmospheric sciences , sulfate , aerosol , ozone , atmosphere (unit) , photodissociation , sulfate aerosol , tropospheric ozone , chemistry , sulfur dioxide , absorption (acoustics) , photochemistry , meteorology , inorganic chemistry , materials science , geology , composite material , physics , organic chemistry
The eruption of Mount Pinatubo in 1991 injected a large amount of SO 2 into the stratosphere, which formed sulfate aerosols. Increased scattering and absorption of UV radiation by the enhanced stratospheric SO 2 and aerosols decreased the amount of UV radiation reaching the troposphere, causing changes in tropospheric photochemistry. These changes affected the oxidizing capacity of the atmosphere and the removal rate of CH 4 in the years following the eruption. We use the three‐dimensional chemistry transport model TM5 coupled to the aerosol microphysics module M7 to simulate the evolution of SO 2 and sulfate aerosols from the Pinatubo eruption. Their effect on tropospheric photolysis frequencies and concentrations of OH and CH 4 is quantified for the first time. We find that UV attenuation by stratospheric sulfur decreased the photolysis frequencies of both ozone and NO 2 by about 2% globally, decreasing global OH concentrations by a similar amount in the first 2 years after the eruption. SO 2 absorption mainly affects OH primary production by ozone photolysis, while aerosol scattering also alters OH recycling. The effect of stratospheric sulfur on global OH and CH 4 is dominated by the effect of aerosol extinction, while SO 2 absorption contributes by 12.5% to the overall effect in the first year after the eruption. The reduction in OH concentrations causes an increase in the CH 4 growth rate of 4 and 2 ppb/yr in the first and second years after the eruption, respectively, contributing 11 Tg to the 27 Tg observed CH 4 burden change in late 1991 and early 1992.