Abstract
On the role of vibrationally excited H2 as a source of OH in the mesosphere
Department of Chemistry, University of Nevada Las Vegas, Las Vegas, Nevada, USA
It has recently been suggested that the reaction between vibrationally excited H2(v = 1) and O(3 P) atoms may be an important source of OH in the upper mesosphere. Here, we report accurate quantum calculations of rate coefficients for the O(3 P) + H2(v = 1) reaction and show that the proposed mechanism is not an important source of OH in the mesosphere. Our calculation employs chemically accurate potential energy surfaces for the O + H2 system and quantum mechanical method for the calculation of the relevant cross sections and rate coefficients.
Received 12 November 2003; accepted 16 December 2003; published 21 February 2004.
Citation: (2004), On the role of vibrationally excited H2 as a source of OH in the mesosphere, Geophys. Res. Lett., 31, L04106, doi:10.1029/2003GL019059.
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