Statistical inference of OH concentrations and air mass dilution rates from successive observations of nonmethane hydrocarbons in single air masses

被引:27
作者
Arnold, S. R.
Methven, J.
Evans, M. J.
Chipperfield, M. P.
Lewis, A. C.
Hopkins, J. R.
McQuaid, J. B.
Watson, N.
Purvis, R. M.
Lee, J. D.
Atlas, E. L.
Blake, D. R.
Rappenglueck, B.
机构
[1] Univ Leeds, Sch Earth & Environm, Inst Atmospher Sci, Leeds LS2 9JT, W Yorkshire, England
[2] Univ Reading, Dept Meteorol, Reading RG6 6BB, Berks, England
[3] Univ York, Dept Chem, York YO10 5DD, N Yorkshire, England
[4] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Div Marine & Atmospher Chem, Miami, FL 33149 USA
[5] Forschungszentrum Karlsruhe, Inst Meteorol & Climate Res, D-82467 Garmisch Partenkirchen, Germany
[6] Univ Calif Irvine, Dept Chem, Irvine, CA 92697 USA
基金
英国自然环境研究理事会;
关键词
D O I
10.1029/2006JD007594
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
[1] Bayesian inference has been used to determine rigorous estimates of hydroxyl radical concentrations ([(OH) over bar]) and air mass dilution rates ( K) averaged following air masses between linked observations of nonmethane hydrocarbons (NMHCs) spanning the North Atlantic during the Intercontinental Transport and Chemical Transformation (ITCT)- Lagrangian-2K4 experiment. The Bayesian technique obtains a refined ( posterior) distribution of a parameter given data related to the parameter through a model and prior beliefs about the parameter distribution. Here, the model describes hydrocarbon loss through OH reaction and mixing with a background concentration at rate K. The Lagrangian experiment provides direct observations of hydrocarbons at two time points, removing assumptions regarding composition or sources upstream of a single observation. The estimates are sharpened by using many hydrocarbons with different reactivities and accounting for their variability and measurement uncertainty. A novel technique is used to construct prior background distributions of many species, described by variation of a single parameter a. This exploits the high correlation of species, related by the first principal component of many NMHC samples. The Bayesian method obtains posterior estimates of [(OH) over bar], K and alpha following each air mass. Median [(OH) over bar] values are typically between 0.5 and 2.0 x 10(6) molecules cm(-3), but are elevated to between 2.5 and 3.5 x 10(6) molecules cm(-3), in low-level pollution. A comparison of [(OH) over bar] estimates from absolute NMHC concentrations and NMHC ratios assuming zero background ( the "photochemical clock'' method) shows similar distributions but reveals systematic high bias in the estimates from ratios. Estimates of K are similar to 0.1 day(-1) but show more sensitivity to the prior distribution assumed.
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页数:15
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