Concentrations of OH in the atmosphere are extremely small, and for any quantitative measurement technique it is imperative that the observed signal originates solely from ambient OH. A master equation model has been formulated to calculate the contribution to the OH concentration from laser photolysis of O 3 and the subsequent reaction of O(¹D) with H 2 O, for conditions typical of instruments designed to measure OH by laser‐induced fluorescence. The model incorporates the quantum state specific production of OH from the O(¹D)+H 2 O reaction and rotational energy transfer, and calculates the temporal behaviour of all rotational states. For detection at 308 nm and 282 nm, whilst probing the lowest rotational level, N”=1, the model predicts that interference from laser generated OH accounts for 0.4% and ∼10% respectively, of the total LIF signal, for [OH]=10 6 molecules cm −3 , [O 3 ]=50 ppb, 40% relative humidity, and typical operating temperatures, pressures and laser parameters.
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Zeng et al. (1998) studied this question.
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