Aircraft vertical profiles of trace gas and aerosol pollution over the mid-Atlantic United States: Statistics and meteorological cluster analysis

被引:92
作者
Taubman, BF
Hains, JC
Thompson, AM
Marufu, LT
Doddridge, BG
Stehr, JW
Piety, CA
Dickerson, RR
机构
[1] Penn State Univ, Dept Meteorol, University Pk, PA 16802 USA
[2] Univ Maryland, Dept Chem & Biochem, College Pk, MD 20742 USA
[3] Univ Maryland, Dept Meteorol, College Pk, MD 20742 USA
关键词
D O I
10.1029/2005JD006196
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
From 1997 to 2003, airborne measurements of O-3, CO, SO2, and aerosol properties were made during summertime air pollution episodes over the mid-Atlantic United States (34.7-44.6 degrees N, 68.4-81.6 degrees W) as part of the Regional Atmospheric Measurement, Modeling, and Prediction Program (RAMMPP). Little diurnal variation was identified in the CO, SO2, and Angstrom exponent profiles, although the Angstrom exponent profiles decreased with altitude. Boundary layer O-3 was greater in the afternoon, while lower free tropospheric O-3 was invariant at similar to 55 ppbv. The single scattering albedo increased from morning to afternoon (0.93 +/- 0.01-0.94 +/- 0.01); however, both profiles decreased with altitude. A cluster analysis of back trajectories in conjunction with the vertical profile data was used to identify source regions and characteristic transport patterns during summertime pollution episodes. When the greatest trajectory density lay over the northern Ohio River Valley, the result was large O-3 values, large SO2/CO ratios, highly scattering particles, and large aerosol optical depths. Maximum trajectory density over the southern Ohio River Valley resulted in little pollution. The greatest afternoon O-3 values occurred during periods of stagnation. North-northwesterly and northerly flow brought the least pollution overall. The contribution of regional transport to afternoon boundary layer O-3 was quantified. When the greatest cluster trajectory density lay over the Ohio River Valley (similar to 59% of the profiles), transport accounted for 69-82% of the afternoon boundary layer O-3. Under stagnant conditions (similar to 27% of the profiles), transport only accounted for 58% of the afternoon boundary layer O-3. The results from this study provide a description of regional chemical and transport processes that will be valuable to investigators from the Baltimore, New York, and Pittsburgh EPA Supersites.
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