OH and HO2concentrations, sources, and loss rates during the Southern Oxidants Study in Nashville, Tennessee, summer 1999

التفاصيل البيبلوغرافية
العنوان: OH and HO2concentrations, sources, and loss rates during the Southern Oxidants Study in Nashville, Tennessee, summer 1999
المؤلفون: Richard E. Shetter, Eric J. Williams, James M. Roberts, Jeremy N. Bassis, C. A. Stroud, Jochen Stutz, T. A. Kovacs, V. Young, Hartwig Harder, R. Lesher, Gregory J. Frost, James B. Simpas, Bertram T. Jobson, Samuel R. Hall, Alan Fried, William H. Brune, Monica Martinez, Robert J. Zamora, B. Alicke, Allen B. White, B. Wert
المصدر: Journal of Geophysical Research. 108
بيانات النشر: American Geophysical Union (AGU), 2003.
سنة النشر: 2003
مصطلحات موضوعية: Atmospheric Science, Daytime, Ozone, Ecology, Meteorology, Analytical chemistry, Paleontology, Soil Science, Forestry, Aquatic Science, Oceanography, Trace gas, Troposphere, chemistry.chemical_compound, Geophysics, chemistry, Space and Planetary Science, Geochemistry and Petrology, Photostationary state, Earth and Planetary Sciences (miscellaneous), Mixing ratio, Steady state (chemistry), NOx, Earth-Surface Processes, Water Science and Technology
الوصف: [1] OH and HO2 mixing ratios and total OH reactivity were measured together with photolysis frequencies, NOx, O3, many VOCs, and other trace gases during the midsummer 1999 SOS campaign in Nashville, Tennessee. These measurements provided an excellent opportunity to study OH and HO2 (collectively called HOx), and their sources and sinks in a polluted metropolitan environment. HOx generally showed the expected diurnal evolution, with maxima around noon of up to about 0.8 pptv of OH and 80 pptv of HO2 during sunny days. Overall, daytime observed OH and HO2 were a factor of 1.33 and 1.56 times modeled values, within the combined 2σ instrument and model uncertainties. The chain length of HOx, which is determined from the ratio of the measured total OH reactivity that cycles OH to the total HOx loss, was on average 3–8 during daytime and up to 3 during nighttime, in general agreement with expectations. However, differences occurred between observed HOx behavior and expectations from theory and models. First, HO2 was greater than expected during daytime when NO mixing ratios were high; ozone production did not decrease as expected when NO was greater than 2 ppbv. Ozone production determined by the imbalance of the NOx photostationary state, which was almost twice that from HO2, also shows this dependence on NO. Second, the calculated OH production rate, which should equal the measured OH loss rate because OH is in steady state, is instead less than the measured OH loss rate by (1–2) × 107 molecules cm-3 s-1, with low statistical significance during the day and high statistical significance at night. Third, surprisingly high OH and HO2 mixing ratios were often observed during nighttime. The nighttime OH mixing ratio and the HO2/OH ratio cannot be explained by known reaction mechanisms, even those involving O3 and alkenes. Because instrument tests have failed to reveal any instrument artifacts, more exotic chemicals or chemistry, such as OH adducts or other radicals that fall apart into OH inside the instrument, are suspected.
تدمد: 0148-0227
DOI: 10.1029/2003jd003551
URL الوصول: https://explore.openaire.eu/search/publication?articleId=doi_________::2a5b193648c281e9d29c2900dd12ed51
https://doi.org/10.1029/2003jd003551
Rights: OPEN
رقم الانضمام: edsair.doi...........2a5b193648c281e9d29c2900dd12ed51
قاعدة البيانات: OpenAIRE
الوصف
تدمد:01480227
DOI:10.1029/2003jd003551