HOxchemistry during INTEX-A 2004: Observation, model calculation, and comparison with previous studies
| Autor: | Alan Fried, Melody A. Avery, William H. Brune, Donald R. Blake, Hanwant B. Singh, Xinrong Ren, Robert Bryan Long, John D. W. Barrick, Paul O. Wennberg, Brian G. Heikes, Ronald C. Cohen, Glenn S. Diskin, R. Shetter, Gao Chen, L. Greg Huey, James H. Crawford, Jingqiu Mao, Zhong Chen, Glen W. Sachse, Jennifer R. Olson |
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| Rok vydání: | 2008 |
| Předmět: |
Atmospheric Science
Ozone Ecology Meteorology Planetary boundary layer Paleontology Soil Science Forestry Aquatic Science Oceanography Atmospheric sciences Atmosphere Troposphere chemistry.chemical_compound Geophysics chemistry Space and Planetary Science Geochemistry and Petrology Atmospheric chemistry Middle latitudes Earth and Planetary Sciences (miscellaneous) Hydroxyl radical Isoprene Earth-Surface Processes Water Science and Technology |
| Zdroj: | Journal of Geophysical Research: Atmospheres. 113 |
| ISSN: | 0148-0227 |
| DOI: | 10.1029/2007jd009166 |
| Popis: | OH and HO2 were measured with the Airborne Tropospheric Hydrogen Oxides Sensor (ATHOS) as part of a large measurement suite from the NASA DC-8 aircraft during the Intercontinental Chemical Transport Experiment - A (INTEX-A). This mission, which was conducted mainly over North America and the western Atlantic Ocean in summer 2004, was an excellent test of atmospheric oxidation chemistry. Throughout the troposphere, observed OH was generally 0.60 of the modeled OH; below 8 km, observed HO2 was generally 0.78 of modeled HO2. If the over-prediction of tropospheric OH is not due to an instrument calibration error, then it implied less global tropospheric oxidation capacity and longer lifetimes for gases like methane and methyl chloroform than currently thought. This discrepancy falls well outside uncertainties in both the OH measurement and rate coefficients for known reactions and points to a large unknown OH loss. If the modeled OH is forced to agree with observed values by introducing of an undefined OH loss that removed HOx (HOx=OH+HO2), the observed and modeled HO2 and HO2/OH ratios are largely reconciled within the measurement uncertainty. HO2 behavior above 8 km was markedly different. The observed-to-modeled ratio correlating with NO. The observed-to-modeled HO2 ratio increased from approximately 1 at 8 km to more than approximately 2.5 at 11 km with the observed-to-modeled ratio correlating with NO. The observed-to-modeled HO2 and NO were both considerably greater than observations from previous campaigns. In addition, the observed-to-modeled HO2/OH, which is sensitive to cycling reactions between OH and HO2, increased from approximately 1.2 at 8 km to almost 4 above 11 km. In contrast to the lower atmosphere, these discrepancies above 8 km suggest a large unknown HOx source and additional reactants that cycle HOx from OH to HO2. In the continental planetary boundary layer, the OH observed-to-modeled ratio increased from 0.6 when isoprene was less than 0.1 ppbv to over 3 when isoprene was greater than 2 ppbv, suggesting that forests throughout the United States are emitting unknown HOx sources. Progress in resolving these discrepancies requires further examinations of possible unknown OH sinks and HOx sources and a focused research activity devoted to ascertaining the accuracy of the OH and HO2 measurements. |
| Databáze: | OpenAIRE |
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