Aircraft measurements of the latitudinal, vertical, and seasonal variations of NMHCs, methyl nitrate, methyl halides, and DMS during the First Aerosol Characterization Experiment (ACE 1)

被引:82
作者
Blake, NJ [1 ]
Blake, DR
Wingenter, OW
Sive, BC
Kang, CH
Thornton, DC
Bandy, AR
Atlas, E
Flocke, F
Harris, JM
Rowland, FS
机构
[1] Univ Calif Irvine, Dept Chem, Irvine, CA 92697 USA
[2] Jeju Natl Univ, Dept Chem, Cheju 690756, South Korea
[3] Drexel Univ, Dept Chem, Philadelphia, PA 19104 USA
[4] Natl Ctr Atmospher Res, Div Atmospher Chem, Boulder, CO 80307 USA
[5] NOAA, Climate Monitoring & Diagnost Lab, Boulder, CO 80303 USA
关键词
D O I
10.1029/1999JD900238
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Canister sampling for the determination of atmospheric mixing ratios of nonmethane hydrocarbons (NMHCs), selected halocarbons, and methyl nitrate was conducted aboard the National Center for Atmospheric Research (NCAR) C-130 aircraft over the Pacific and Southern Oceans as part of the First Aerosol Characterization Experiment (ACE 1) during November and December 1995. A latitudinal profile, flown from 76 degrees N to 60 degrees S, revealed latitudinal gradients for most trace gases. NMHC and halocarbon gases with predominantly anthropogenic sources, including ethane, ethyne, and tetrachloroethene, exhibited significantly higher mixing ratios in the northern hemisphere at all altitudes. Methyl chloride exhibited its lowest mixing ratios at the highest northern hemisphere latitudes, and the distributions of methyl nitrate and methyl iodide were consistent with tropical and subtropical oceanic sources. Layers containing continental air characteristic of aged biomass burning emissions were observed above about 3 km over the remote southern Pacific and near New Zealand between approximately 19 degrees S and 43 degrees S. These plumes originated from the west, possibly from fires in southern Africa. The month-long intensive investigation of the clean marine southern midlatitude troposphere south of Australia revealed decreases in the mixing ratios of ethane, ethyne, propane, and tetrachloroethene, consistent with their seasonal mixing ratio cycle. By contrast, increases in the average marine boundary layer concentrations of methyl iodide, methyl nitrate, and dimethyl sulfide (DMS) were observed as the season progressed to summer conditions. These increases were most appreciable in the region south of 44 degrees S over Southern Ocean waters characterized as subantarctic and polar, indicating a seasonal increase in oceanic productivity for these gases.
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收藏
页码:21803 / 21817
页数:15
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