Potential impact of iodinated replacement compounds CF sub(3)I and CH sub(3)I on atmospheric ozone: a three-dimensional modeling study

• Published in: Atmospheric chemistry and physics discussions Vol. 10; no. 7; pp. 16659 - 16690
• Main Authors: Youn, Daeok, Patten, KO, Wuebbles, D J, Lee, Huikyo, So, Chul-Whan
• Format: Journal Article
• Language: English
• Published: 02.07.2010
• ISSN: 1680-7367; 1680-7375

The concept of Ozone Depletion Potentials (ODPs) is extensively used in policy considerations related to concerns about the effects of various halocarbons and other gases on stratospheric ozone. Many of the recent candidate replacement compounds have atmospheric lifetimes shorter than one year in order to limit their environmental effects, especially on stratospheric ozone. Using a three-dimensional global chemistry-transport model (CTM) of the troposphere and the stratosphere, the purpose of this study is to evaluate the potential effects of several very short-lived iodinated substances, namely iodotrifluoromethane (CF sub(3)I) and methyl iodide (CH sub(3)I), on atmospheric ozone. Like other chemicals with extremely short lifetimes, the stratospheric halogen loading and resulting ozone effects from these compounds are strongly dependent on the location of emissions. For CF sub(3)I, a possible replacement candidate for bromotrifluoromethane (CF sub(3)Br), ODPs derived by the three-dimensional model are 0.008 with chemical lifetime of 5.03 days and 0.016 with a lifetime of 1.13 days for emissions assumed to be evenly distributed over land surfaces at mid-latitudes and the tropics, respectively. While this is the first time the ODPs have been evaluated with a three-dimensional model, these values are in good agreement with those derived previously. The model calculations suggest that tropical convection could deliver a larger portion of the gas and their breakdown products to the upper troposphere and lower stratosphere if emission source is located in the tropics. The resulting ODP for CH sub(3)I, emitted from mid-latitudes, is 0.017 with lifetime of 13.59 days. The validity of our model iodine chemistry to evaluate ODPs of the iodine species is guaranteed with good qualitative agreement between the model derived distribution of background CH sub(3)I, based on global source emission fluxes from previous studies, and available observations especially in vertical profiles.