Articles | Volume 14, issue 7
Atmos. Chem. Phys., 14, 3589–3622, 2014
https://doi.org/10.5194/acp-14-3589-2014
Atmos. Chem. Phys., 14, 3589–3622, 2014
https://doi.org/10.5194/acp-14-3589-2014
Research article
09 Apr 2014
Research article | 09 Apr 2014

Factors controlling variability in the oxidative capacity of the troposphere since the Last Glacial Maximum

L. T. Murray et al.

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Cited articles

Adams, J. M., Constable, J. V. H., Guenther, A. B., and Zimmerman, P.: An estimate of natural volatile organic compound emissions from vegetation since the last glacial maximum, Atmos. Environ., 3, 73–91, 2001.
Alexander, B., Savarino, J., Barkov, N., Delmas, R., and Thiemens, M. H.: Climate driven changes in the oxidation pathways of atmospheric sulfur, Geophys. Res. Lett., 29, 1685, https://doi.org/10.1029/2002GL014879, 2002.
Alexander, B., Savarino, J., Kreutz, K., and Thiemens, M. H.: Impact of preindustrial biomass-burning emissions on the oxidation pathways of tropospheric sulfur and nitrogen, J. Geophys. Res.-Atmos., 109, D08303, https://doi.org/10.1029/2003JD004218, 2004.
Allen, D. J., Pickering, K., Duncan, B., and Damon, M.: Impact of lightning NO emissions on North American photochemistry as determined using the Global Modeling Initiative (GMI) model, J. Geophys. Res.-Atmos., 115, D22301, https://doi.org/10.1029/2010JD014062, 2010.
Anklin, M. and Bales, R. C.: Recent increase in H2O2 concentration at Summit, Greenland, J. Geophys. Res.-Atmos., 102, 19099–19104, 1997.
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