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Volume 10, issue 3
Atmos. Chem. Phys., 10, 1441–1459, 2010
https://doi.org/10.5194/acp-10-1441-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 10, 1441–1459, 2010
https://doi.org/10.5194/acp-10-1441-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.

  10 Feb 2010

10 Feb 2010

Measurements of OH and HO2 yields from the gas phase ozonolysis of isoprene

T. L. Malkin et al.

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Cited articles

Arneth, A., Monson, R. K., Schurgers, G., Niinemets, Ü., and Palmer, P. I.: Why are estimates of global terrestrial isoprene emissions so similar (and why is this not so for monoterpenes)?, Atmos. Chem. Phys., 8, 4605–4620, 2008.
Asatryan, R. and Bozzelli, J. W.: Formation of a Criegee intermediate in the low-temperature oxidation of dimethyl sulfoxide, Phys. Chem. Chem. Phys., 10, 1769–1780, 2008.
Aschmann, S. M and Atkinson, R.: Formation yields of methyl vinyl ketone and methacrolein from the gas-phase reaction of O3 with isoprene, Environ. Sci. Technol., 28(8), 1539–1542, 1994.
Aschmann, S. M., Arey, J., and Atkinson, R.: OH radical formation from the gas-phase reactions of O3 with methacrolein and methyl vinyl ketone, Atmos. Environ., 30, 2939–2943, 1996.
Atkinson, R. and Aschmann, S. M.: Rate constants for the gas-phase reactions of the OH radical with a series of aromatic hydrocarbons at 296±2 K, Int. J. Chem. Kinet., 21, 355–365, 1989.
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