Measurements of enhanced H2SO4 and 3-4 nm particles near a frontal cloud during the First Aerosol Characterization Experiment (ACE 1)

被引:81
作者
Weber, RJ [1 ]
Chen, G
Davis, DD
Mauldin, RL
Tanner, DJ
Eisele, FL
Clarke, AD
Thornton, DC
Bandy, AR
机构
[1] Georgia Inst Technol, Sch Earth & Atmospher Sci, Atlanta, GA 30332 USA
[2] Drexel Univ, Dept Chem, Philadelphia, PA 19104 USA
[3] Univ Hawaii, Sch Ocean & Earth Sci & Technol, Honolulu, HI 96822 USA
[4] Natl Ctr Atmospher Res, Div Atmospher Chem, Boulder, CO 80303 USA
关键词
D O I
10.1029/2000JD000109
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Observations of new particle production recorded near a frontal cloud at similar to6 km above sea level in a remote marine region are reported. Two distinct locations situated near the cloud were found to have enhanced concentrations of sulfuric acid vapor (H2SO4) and freshly formed 3-4 nm particles. Both were in droplet-free air situated above cloudy regions. No evidence for enhanced H2SO4 or nucleation was observed in clear air far from the cloud. In the nucleating region the aerosol size distribution from 3 nm to 600 mum was observed to be trimodal, with a prominent ultrafine mode, and was qualitatively, similar to surface-based measurements recorded in regions of postfrontal subsidence. The measurements support the notion that new particle production in the free troposphere occurs preferentially in clear air near clouds via enhanced photochemical production of nucleation precursor gases and that H2SO4 participates. A model simulation suggested that a doubling of ultraviolet intensities above the cloud due to cloud enhanced up-welling radiation or reasonable enhancements in sulfur dioxide concentrations could account for the higher H2SO4 concentration observed near the cloud. In the nucleation regions, H2SO4 and water vapor concentrations were too low for binary nucleation of sulfuric acid and water, according to current nucleation models. The mechanisms of particle formation and growth remain uncertain. The measurements were part of the first Aerosol Characterization Experiment (ACE 1) conducted in the remote South Pacific Ocean (153 degreesE, 47 degreesS) on November 27, 1995.
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页码:24107 / 24117
页数:11
相关论文
共 39 条
[1]   Laboratory studies of particle nucleation:: Initial results for H2SO4, H2O, and NH3 vapors [J].
Ball, SM ;
Hanson, DR ;
Eisele, FL ;
McMurry, PH .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D19) :23709-23718
[2]   International Global Atmospheric Chemistry (IGAC) project's first aerosol characterization experiment (ACE 1): Overview [J].
Bates, TS ;
Huebert, BJ ;
Gras, JL ;
Griffiths, FB ;
Durkee, PA .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1998, 103 (D13) :16297-16318
[3]  
Berresheim H., 1995, COMPOSITION CHEM CLI, P251
[4]   Is aerosol production within the remote marine boundary layer sufficient to maintain observed concentrations? [J].
Capaldo, KP ;
Kasibhatla, P ;
Pandis, SN .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1999, 104 (D3) :3483-3500
[5]   Atmospheric nuclei and related aerosol fields over the Atlantic: Clean subsiding air and continental pollution during ASTEX [J].
Clarke, AD ;
Uehara, T ;
Porter, JN .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1997, 102 (D21) :25281-25292
[6]   ATMOSPHERIC NUCLEI IN THE REMOTE FREE-TROPOSPHERE [J].
CLARKE, AD .
JOURNAL OF ATMOSPHERIC CHEMISTRY, 1992, 14 (1-4) :479-488
[7]   Particle production in the remote marine atmosphere: Cloud outflow and subsidence during ACE 1 [J].
Clarke, AD ;
Varner, JL ;
Eisele, F ;
Mauldin, RL ;
Tanner, D ;
Litchy, M .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1998, 103 (D13) :16397-16409
[8]   Particle production near marine clouds: Sulfuric acid and predictions from classical binary nucleation [J].
Clarke, AD ;
Kapustin, VN ;
Eisele, FL ;
Weber, RJ ;
McMurry, PH .
GEOPHYSICAL RESEARCH LETTERS, 1999, 26 (16) :2425-2428
[9]  
COAKLEY JA, 1983, J ATMOS SCI, V40, P116, DOI 10.1175/1520-0469(1983)040<0116:TEOTAO>2.0.CO
[10]  
2