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

Geophysical Research Letters

Volumn 24, Issue 24, 1997, Pages 3185-3188

  Folkins, Ian ^a   Wennberg, P O ^b   Hanisco, T F ^b   Anderson, J G ^b   Salawitch, R J ^c  

^a DALHOUSIE UNIVERSITY   (Canada)

^b HARVARD UNIVERSITY   (United States)

^c CALIFORNIA INSTITUTE OF TECHNOLOGY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ACETONE; BUDGET CONTROL; NITROGEN OXIDES; OZONE; TROPOSPHERE; BIOMASS; COMBUSTION; MODELS; PHOTOCHEMICAL REACTIONS; THERMAL PLUMES; WATER;

BIOMASS-BURNING; CH 4; NO X; OZONE PRODUCTION; PLUME SOURCE; PRODUCTION RATES; UPPER TROPOSPHERE;

PHOTOLYSIS; EARTH ATMOSPHERE;

HYDROXYL RADICAL;

ATMOSPHERIC PLUME; BIOMASS BURNING; HYDROPEROXYL RADICAL; HYDROXYL; NITRIC OXIDE; OZONE PRODUCTION;

EID: 0031393693     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/97GL03047     Document Type: Article

References (12)

1. Chatfield, R. B., and P. J. Crutzen, Sulfur dioxide in remote oceanic air: Cloud transport of reactive precursors, J. Geophys. Res., 89, 7111-7132, 1984.
2. DeMore et al., Chemical kinetics and photochemical data for use in stratospheric modeling: evaluation number 11, JPL Publication 94-26, 1994.
3. Fahey, D. W. et al., In-situ measurements of total reactive nitrogen, total water, and aerosol in polar stratospheric clouds in the Antarctic stratosphere, J. Geophys. Res. 94, 11299-11315, 1989.
4. Folkins, I., R. B. Chatfield, D. Baumgardner, and M. Proffitt, Biomass burning and deep convection in Southeast Asia: results from ASHOE/MAESA, J. Geophys. Res., 102, 13291-13299, 1997.
5. 2 in the upper troposphere suggest a major source from convective injection of peroxides, Geophys. Res. Lett., this issue.
6. Kousky, V. E., Climate Diagnostics Bulletin May 1994, U. S. Department of Commerce, 1994.
7. McKeen, S. A., et al., The photochemistry of acetone in the upper troposphere: A source of odd-hydrogen radicals, Geophys. Res. Lett., this issue.
8. Pickering, K. E., et al., Convective transport of biomass burning emissions over Brazil during TRACE A, J. Geophys. Res., 101, 23993-24012, 1996.
9. x photochemistry of the upper troposphere driven by deep tropical convection, Geophys. Res. Lett., this issue.
10. Singh, H. B., M. Kanakidou, P. J. Crutzen, and D. J. Jacob, High concentration and photochemical fate of oxygenated hydrocarbons in the global troposphere, Nature 378, 50-54, 1995.
11. Thompson, A. M. et al., K. E. Pickering, D. P. McNamara, M. R. Schoeberl, R. D. Hudson, J. H. Kim, E. V. Browell, V. W. J. H. Kirchhoff, and D. Nganga, Where did tropospheric ozone over southern Africa and the tropical Atlantic come from in October 1992? Insights from TOMS, GTE TRACE A, and SAFARI 1992, J. Geophys. Res. , 101, 24251-24278, 1996.
12. Wennberg, P. O., et al., Hydrogen radicals, nitrogen radicals, and the production of ozone in the middle and upper troposphere, submitted to Science, 1997.