Open AccessAnthropogenic forcing on tropospheric ozone and OH since preindustrial times
Author(s) -
Wang Yuhang,
Jacob Daniel J.
Publication year - 1998
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/1998jd100004
Subject(s) - troposphere , atmospheric sciences , tropospheric ozone , combustion , ozone , climatology , forcing (mathematics) , radiative forcing , environmental science , hydrocarbon , atmosphere (unit) , chemistry , meteorology , geology , aerosol , geography , organic chemistry
A global three‐dimensional model of tropospheric chemistry is used to investigate the changes in tropospheric O 3 and OH since preindustrial times as a result of fuel combustion and industry, biomass burning, and growth in atmospheric CH 4 . Model results indicate a 63% increase of the global tropospheric O 3 burden from preindustrial times to present (80% and 50% in the northern and southern hemispheres, respectively). Anthropogenic emissions of NO x and of CO and hydrocarbons make comparable contributions to the global O 3 increase (60% and 40% respectively), even though the local rate of tropospheric O 3 production is generally NO χ limited. The rise in O 3 production parallels closely the rise in the emissions of CO and hydrocarbon because the O 3 yield per mole of CO or hydrocarbon oxidized has remained constant at 0.7–0.8 mol/mol since preindustrial times. In contrast, the O 3 production efficiency per mole of NO χ emitted has decreased globally by a factor of 2. We find a 9% decrease in the global mean OH concentration (mass‐weighted) since preindustrial times. A linear relationship is found in the model between the global mean OH concentration and the S N /S C 3/2 ratio, where S N and S C are the sources of NO χ and of CO and hydrocarbons, respectively. The relative constancy of the global mean OH concentration since preindustrial times reflects the conservation of the S N /S C 3/2 ratio despite large increases in both S N and S C . Comparisons of model results with reconstructed nineteenth century observations of O 3 at continental sites indicate a systematic overestimate of about 5 ppbv. Correcting this overestimate would require either a large missing chemical sink for O 3 or a downward revision of the natural NO χ source from lightning (3 Tg N yr −1 in our model). The nineteenth century observations of O 3 over France show no vertical gradient between the boundary layer and the free troposphere, which is inconsistent with our current understanding of tropospheric O 3 . The model underestimates preindustrial CO concentrations derived from polar ice cores; these measurements are difficult to reconcile with any reasonable CO emission inventories.