Influence of biomass combustion emissions on the distribution of acidic trace gases over the southern Pacific basin during austral springtime

被引:41
作者
Talbot, RW [1 ]
Dibb, JE
Scheuer, EM
Blake, DR
Blake, NJ
Gregory, GL
Sachse, GW
Bradshaw, JD
Sandholm, ST
Singh, HB
机构
[1] Univ New Hampshire, Inst Study Earth Oceans & Space, Durham, NH 03824 USA
[2] Univ Calif Irvine, Dept Chem, Irvine, CA 92717 USA
[3] NASA, Langley Res Ctr, Hampton, VA 23665 USA
[4] Georgia Inst Technol, Dept Earth & Atmospher Sci, Atlanta, GA 30332 USA
[5] NASA, Ames Res Ctr, Moffett Field, CA 94035 USA
关键词
D O I
10.1029/98JD00879
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This paper describes the large-scale distributions of HNO3, HCOOH, and CH3COOH over the central and South Pacific basins during the Pacific Exploratory Mission-Tropics (PEM-Tropics) in austral springtime. Because of the remoteness of this region from continental areas, low part per trillion by volume (pptv) mixing ratios of acidic gases were anticipated to be pervasive over the South Pacific basin. However,; at altitudes of 2-12 km over the South Pacific, air parcels were encountered frequently with significantly enhanced mixing ratios (up to 1200 pptv) of acidic gases. Most of these air parcels were centered in the 3-7 km altitude range and occurred within the 15 degrees-65 degrees S latitudinal band. The acidic gases exhibited an overall general correlation with CH3Cl, PAN, and O-3, suggestive of photochemical and biomass burning sources. There was no correlation or trend of acidic gases with common industrial tracer compounds (e.g., C2Cl4 or CH3CCl3). The combustion emissions sampled over the South Pacific basin were relatively aged exhibiting C2H2/CO ratios in the range of 0.2-2.2 pptv/ppbv. The relationships between acidic gases and this ratio were similar to what was observed in aged air parcels (i.e., >3-5 days since they were over a continental area) over the western North Pacific during the Pacific Exploratory Mission-West Phases A and B (PEM-West A and B). In the South Pacific marine boundary layer a median C2H2/CO ratio of 0.6 suggested that this region was generally not influenced by direct inputs of biomass combustion emissions. Here we observed the lowest mixing ratios of acidic gases, with median values of 14 pptv for HNO3, 19 pptv for HCOOH, and 18 pptv for CH3COOH. These values were coincident with low mixing ratios of NOx (<10 pptv), CO (approximate to 50 parts per billion by volume (ppbv)), O-3 (< 20 ppbv), and long-lived hydrocarbons (e.g., C2H6 <300 pptv). Overall, the PEM-Tropics data suggest an important influence of aged biomass combustion emissions on the distributions of acidic gases over the South Pacific basin in austral springtime.
引用
收藏
页码:5623 / 5634
页数:12
相关论文
共 30 条
[1]   FORMIC AND ACETIC-ACID OVER THE CENTRAL AMAZON REGION, BRAZIL .1. DRY SEASON [J].
ANDREAE, MO ;
TALBOT, RW ;
ANDREAE, TW ;
HARRISS, RC .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1988, 93 (D2) :1616-1624
[2]   PRECIPITATION CHEMISTRY IN CENTRAL AMAZONIA [J].
ANDREAE, MO ;
TALBOT, RW ;
BERRESHEIM, H ;
BEECHER, KM .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1990, 95 (D10) :16987-16999
[3]   GASEOUS OXYGENATED HYDROCARBONS IN THE REMOTE MARINE TROPOSPHERE [J].
ARLANDER, DW ;
CRONN, DR ;
FARMER, JC ;
MENZIA, FA ;
WESTBERG, HH .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1990, 95 (D10) :16391-16403
[4]   Biomass burning emissions and vertical distribution of atmospheric methyl halides and other reduced carbon gases in the South Atlantic region [J].
Blake, NJ ;
Blake, DR ;
Sive, BC ;
Chen, TY ;
Rowland, FS ;
Collins, JE ;
Sachse, GW ;
Anderson, BE .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D19) :24151-24164
[5]   SEASONAL DISTRIBUTION OF AFRICAN SAVANNA FIRES [J].
CAHOON, DR ;
STOCKS, BJ ;
LEVINE, JS ;
COFER, WR ;
ONEILL, KP .
NATURE, 1992, 359 (6398) :812-815
[6]   AQUEOUS-PHASE SOURCE OF FORMIC-ACID IN CLOUDS [J].
CHAMEIDES, WL ;
DAVIS, DD .
NATURE, 1983, 304 (5925) :427-429
[7]   Asian influence over the western North Pacific during the fall season: Inferences from lead 210, soluble ionic species and ozone [J].
Dibb, JE ;
Talbot, RW ;
Klemm, KI ;
Gregory, GL ;
Singh, HB ;
Bradshaw, JD ;
Sandholm, ST .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D1) :1779-1792
[8]   Biomass burning signatures in the atmosphere and snow at Summit, Greenland: An event on 5 August 1994 [J].
Dibb, JE ;
Talbot, RW ;
Whitlow, SI ;
Shipham, MC ;
Winterle, J ;
McConnell, J ;
Bales, R .
ATMOSPHERIC ENVIRONMENT, 1996, 30 (04) :553-561
[9]   O-3, NOY, AND NOX/NOY IN THE UPPER TROPOSPHERE OF THE EQUATORIAL PACIFIC [J].
FOLKINS, IA ;
WEINHEIMER, AJ ;
RIDLEY, BA ;
WALEGA, JG ;
ANDERSON, B ;
COLLINS, JE ;
SACHSE, G ;
PUESCHEL, RF ;
BLAKE, DR .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1995, 100 (D10) :20913-20926
[10]  
HALES JM, 1979, ATMOS ENVIRON, V12, P389