Physical characterization of aerosol particles during nucleation events

被引:312
作者
Aalto, P
Hämeri, K
Becker, E
Weber, R
Salm, J
Mäkelä, JM
Hoell, C
O'Dowd, CD
Karlsson, H
Hansson, HC
Väkevä, M
Koponen, IK
Buzorius, G
Kulmala, M
机构
[1] Univ Helsinki, Dept Phys, FIN-00014 Helsinki, Finland
[2] Univ Sunderland, Sch Environm, Ctr Marine & Atmospher Sci, Sunderland SR2 7BW, England
[3] Georgia Inst Technol, Sch Earth & Atmospher Sci, Atlanta, GA 30332 USA
[4] Univ Tartu, Inst Environm Phys, EE-50090 Tartu, Estonia
[5] Stockholm Univ, Inst Appl Environm Res, SE-10691 Stockholm, Sweden
来源
TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY | 2001年 / 53卷 / 04期
关键词
D O I
10.1034/j.1600-0889.2001.530403.x
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Particle concentrations and size distributions have been measured from different heights inside and above a boreal forest during three BIOFOR campaigns (14 April-22 May 1998, 27 July-21 August 1998 and 20 March-24 April 1999) in Hyytiala, Finland. Typically, the shape of the background distribution inside the forest exhibited 2 dominant modes: a fine or Aitken mode with a geometric number mean diameter of 44 nm and a mean concentration of 1160 cm(-3) and an accumulation mode with mean diameter of 154 nm and a mean concentration of 830 cm(-3). A coarse mode was also present, extending up to sizes of 20 mum having a number concentration of 1.2 cm(-3), volume mean diameter of 2.0 mum and a geometric standard deviation of 1.9. Aerosol humidity was lower than 50% during the measurements. Particle production was observed on many days, typically occurring in the late morning. Under these periods of new particle production, a nucleation mode was observed to form at diameter of the order of 3 nm and, on most occasions, this mode was observed to grow into Aitken mode sizes over the course of a day. Total concentrations ranged from 410-45000 cm(-3), the highest concentrations occurring on particle production days. A clear gradient was observed between particle concentrations encountered below the forest canopy and those above, with significantly lower concentrations occurring within the canopy. Above the canopy, a slight gradient was observed between 18 in and 67 in, with at maximum 5% higher concentration observed at 67 in during the strongest concentration increases.
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页码:344 / 358
页数:15
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