Tropospheric O3from photolysis of O2

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Tropospheric O3 from photolysis of O2

[1] Photolytic dissociation of molecular oxygen (O2) at wavelengths about 205 nm produces ozone (O3) in the upper tropical troposphere. In tropospheric chemistry models that ignore this process, the O3 abundance above 14 km in the tropics (a.k.a. Tropopause Transition Layer) is underestimated by 5 to 20 ppb. Even for models including O2 photolysis, uncertainty in the O2 cross sections yields si...

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Tropospheric Aerosol Impacts on Trace-Gas Budgets through Photolysis

Aerosols affect the global budgets of O3, OH and CH4 in part through their alteration of photolysis rates and in part through their direct chemistry interactions with gases (a.k.a. “heterogeneous chemistry”). The first effect is evaluated here with a global tropospheric chemistry transport model using recently developed global climatologies of tropospheric aerosols: a satellite-derived aerosol ...

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ژورنال

عنوان ژورنال: Geophysical Research Letters

سال: 2009

ISSN: 0094-8276

DOI: 10.1029/2008gl036851