OH, HO2, and NO in two biomass burning plumes: Sources of HOxand implications for ozone production

Author:

Folkins Ian,Wennberg P. O.,Hanisco T. F.,Anderson J. G.,Salawitch R. J.

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference12 articles.

1. Sulfur dioxide in remote oceanic air: Cloud transport of reactive precursors;Chatfield;J. Geophys. Res.,1984

2. DeMore Chemical kinetics and photochemical data for use in stratospheric modeling: evaluation number 11 JPL Publication 94-26 1994

3. In-situ measurements of total reactive nitrogen, total water, and aerosol in polar stratospheric clouds in the Antarctic stratosphere;Fahey;J. Geophys. Res.,1989

4. Biomass burning and deep convection in Southeast Asia: results from ASHOE/MAESA;Folkins;J. Geophys. Res.,1997

5. Observed OH and HO2 in the upper troposphere suggest a major source from convective injection of peroxides;Jaeglé;Geophys. Res. Lett.

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