Chemical composition of Asian continental outflow over the western Pacific: Results from Transport and Chemical Evolution over the Pacific (TRACE-P)

Chemical composition of Asian continental outflow over the western Pacific: Results from Transport and Chemical Evolution over the Pacific (TRACE-P). Russo, R., S., Talbot, R., W., Dibb, J., E., Scheuer, E., Seid, G., Jordan, C., E., Fuelberg, H., E., Sachse, G., W., Avery, M., A., Vay, S., A., Blake, D., R., Blake, N., J., Atlas, E., Fried, A., Sandholm, S., T., Tan, D., Singh, H., B., Snow, J., & Heikes, B., G. Journal of Geophysical Research-Atmospheres, 108(D20):-, 2003.

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[1] We characterize the chemical composition of Asian continental outflow observed during the NASA Transport and Chemical Evolution over the Pacific ( TRACE- P) mission during February - April 2001 in the western Pacific using data collected on the NASA DC-8 aircraft. A significant anthropogenic impact was present in the free troposphere and as far east as 150 degreesE longitude reflecting rapid uplift and transport of continental emissions. Five-day backward trajectories were utilized to identify five principal Asian source regions of outflow: central, coastal, north-northwest (NNW), southeast ( SE), and west-southwest (WSW). The maximum mixing ratios for several species, such as CO, C2Cl4, CH3Cl, and hydrocarbons, were more than a factor of 2 larger in the boundary layer of the central and coastal regions due to industrial activity in East Asia. CO was well correlated with C2H2, C2H6, C2Cl4, and CH3Cl at low altitudes in these two regions (r(2) similar to 0.77 - 0.97). The NNW, WSW, and SE regions were impacted by anthropogenic sources above the boundary layer presumably due to the longer transport distances of air masses to the western Pacific. Frontal and convective lifting of continental emissions was most likely responsible for the high altitude outflow in these three regions. Photochemical processing was influential in each source region resulting in enhanced mixing ratios of O-3, PAN, HNO3, H2O2, and CH3OOH. The air masses encountered in all five regions were composed of a complex mixture of photochemically aged air with more recent emissions mixed into the outflow as indicated by enhanced hydrocarbon ratios (C2H2/ CO greater than or equal to 3 and C3H8/C2H6 greater than or equal to 0.2). Combustion, industrial activities, and the burning of biofuels and biomass all contributed to the chemical composition of air masses from each source region as demonstrated by the use of C2H2, C2Cl4, and CH3Cl as atmospheric tracers. Mixing ratios of O-3, CO, C2H2, C2H6, SO2, and C2Cl4 were compared for the TRACE- P and PEM-West B missions. In the more northern regions, O-3, CO, and SO2 were higher at low altitudes during TRACE- P. In general, mixing ratios were fairly similar between the two missions in the southern regions. A comparison between CO/CO2, CO/CH4, C2H6/ C3H8, NOx/SO2, and NOy/(SO2 + nss- SO4) ratios for the five source regions and for the 2000 Asian emissions summary showed very close agreement indicating that Asian emissions were well represented by the TRACE- P data and the emissions inventory.

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 title = {Chemical composition of Asian continental outflow over the western Pacific: Results from Transport and Chemical Evolution over the Pacific (TRACE-P)},
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 abstract = {[1] We characterize the chemical composition of Asian continental outflow observed during the NASA Transport and Chemical Evolution over the Pacific ( TRACE- P) mission during February - April 2001 in the western Pacific using data collected on the NASA DC-8 aircraft. A significant anthropogenic impact was present in the free troposphere and as far east as 150 degreesE longitude reflecting rapid uplift and transport of continental emissions. Five-day backward trajectories were utilized to identify five principal Asian source regions of outflow: central, coastal, north-northwest (NNW), southeast ( SE), and west-southwest (WSW). The maximum mixing ratios for several species, such as CO, C2Cl4, CH3Cl, and hydrocarbons, were more than a factor of 2 larger in the boundary layer of the central and coastal regions due to industrial activity in East Asia. CO was well correlated with C2H2, C2H6, C2Cl4, and CH3Cl at low altitudes in these two regions (r(2) similar to 0.77 - 0.97). The NNW, WSW, and SE regions were impacted by anthropogenic sources above the boundary layer presumably due to the longer transport distances of air masses to the western Pacific. Frontal and convective lifting of continental emissions was most likely responsible for the high altitude outflow in these three regions. Photochemical processing was influential in each source region resulting in enhanced mixing ratios of O-3, PAN, HNO3, H2O2, and CH3OOH. The air masses encountered in all five regions were composed of a complex mixture of photochemically aged air with more recent emissions mixed into the outflow as indicated by enhanced hydrocarbon ratios (C2H2/ CO greater than or equal to 3 and C3H8/C2H6 greater than or equal to 0.2). Combustion, industrial activities, and the burning of biofuels and biomass all contributed to the chemical composition of air masses from each source region as demonstrated by the use of C2H2, C2Cl4, and CH3Cl as atmospheric tracers. Mixing ratios of O-3, CO, C2H2, C2H6, SO2, and C2Cl4 were compared for the TRACE- P and PEM-West B missions. In the more northern regions, O-3, CO, and SO2 were higher at low altitudes during TRACE- P. In general, mixing ratios were fairly similar between the two missions in the southern regions. A comparison between CO/CO2, CO/CH4, C2H6/ C3H8, NOx/SO2, and NOy/(SO2 + nss- SO4) ratios for the five source regions and for the 2000 Asian emissions summary showed very close agreement indicating that Asian emissions were well represented by the TRACE- P data and the emissions inventory.},
 bibtype = {article},
 author = {Russo, R S and Talbot, R W and Dibb, J E and Scheuer, E and Seid, G and Jordan, C E and Fuelberg, H E and Sachse, G W and Avery, M A and Vay, S A and Blake, D R and Blake, N J and Atlas, E and Fried, A and Sandholm, S T and Tan, D and Singh, H B and Snow, J and Heikes, B G},
 journal = {Journal of Geophysical Research-Atmospheres},
 number = {D20}
}

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