Summertime influence of Asian pollution in the free troposphere over North America

Q. Liang (1, 2) , L. Jaeglé (1) , R. C. Hudman (3) , Solène Turquety (4, 3) , D. J. Jacob (3) , M. A. Avery (5) , E. V. Browell (5) , G. W. Sachse (5) , D. R. Blake (6) , W. Brune (7) , X. Ren (7) , R. C. Cohen (8) , J. E. Dibb (9) , A. Fried (10) , H. Fuelberg (11) , M. Porter (11) , B. G. Heikes (12) , G. Huey (13) , H. B. Singh (14) , P. O. Wennberg (15)

1 Department of Atmospheric Sciences [Seattle]
2 GSFC - NASA Goddard Space Flight Center
3 Harvard University
4 SA - Service d'aéronomie
5 LaRC - NASA Langley Research Center [Hampton]
6 UC Irvine - University of California [Irvine]
7 Department of Meteorology and Atmospheric Science [PennState]
8 UC Berkeley - University of California [Berkeley]
9 EOS Climate Change Research Center [Durham]
10 NCAR - National Center for Atmospheric Research [Boulder]
11 FSU - Florida State University [Tallahassee]
12 Department of Oceanography [Narragansett]
13 School of Earth and Atmospheric Sciences [Atlanta]
14 ARC - NASA Ames Research Center
15 CALTECH - California Institute of Technology

We analyze aircraft observations obtained during INTEX-A (1 July to 14 August 2004) to examine the summertime influence of Asian pollution in the free troposphere over North America. By applying correlation analysis and principal component analysis (PCA) to the observations between 6 and 12 km, we find dominant influences from recent convection and lightning (13% of observations), Asia (7%), the lower stratosphere (7%), and boreal forest fires (2%), with the remaining 71% assigned to background. Asian air masses are marked by high levels of CO, O₃, HCN, PAN, C₂H₂, C₆H₆, methanol, and SO₄^2-. The partitioning of NO_y species in the Asian plumes is dominated by PAN (∼600 pptv), with varying NO_x/HNO₃ ratios in individual plumes, consistent with individual transit times of 3-9 days. Export of Asian pollution occurred in warm conveyor belts of midlatitude cyclones, deep convection, and in typhoons. Compared to Asian outflow measurements during spring, INTEX-A observations display lower levels of anthropogenic pollutants (CO, C₃H₈, C₂H₆, C₆H₆) due to shorter summer lifetimes; higher levels of biogenic tracers (methanol and acetone) because of a more active biosphere; and higher levels of PAN, NO_x, HNO₃, and O₃ reflecting active photochemistry, possibly enhanced by efficient NO_y export and lightning. The high ΔO₃/ΔCO ratio (0.76 mol/mol) in Asian plumes during INTEX-A is due to strong photochemical production and, in some cases, mixing with stratospheric air along isentropic surfaces. The GEOS-Chem global model captures the timing and location of the Asian plumes. However, it significantly underestimates the magnitude of observed enhancements in CO, O₃, PAN and NO_x.

Mots clés: Troposphere: constituent transport and chemistry; Pollution: urban and regional; roposphere: composition and chemistry; intercontinental transport; Asia; ozone

Domaines: Planète et Univers [physics]

Q. Liang, L. Jaeglé, R. C. Hudman, Solène Turquety, D. J. Jacob, et al.. Summertime influence of Asian pollution in the free troposphere over North America. Journal of Geophysical Research: Atmospheres, 2007, 112 (D12), ⟨10.1029/2006JD007919⟩. ⟨hal-04110198⟩