Physical characterization of aerosol particles during nucleation events

Citation
P. Aalto et al., Physical characterization of aerosol particles during nucleation events, TELLUS B, 53(4), 2001, pp. 344-358
Citations number
30
Categorie Soggetti
Earth Sciences
Journal title
TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY
ISSN journal
02806509 → ACNP
Volume
53
Issue
4
Year of publication
2001
Pages
344 - 358
Database
ISI
SICI code
0280-6509(200109)53:4<344:PCOAPD>2.0.ZU;2-Q
Abstract
Particle concentrations and size distributions have been measured from diff erent heights inside and above a boreal forest during three BIOFOR campaign s (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 conce ntration of 830 cm(-3). A coarse mode was also present, extending up to siz es of 20 mum having a number concentration of 1.2 cm(-3), volume mean diame ter of 2.0 mum and a geometric standard deviation of 1.9. Aerosol humidity was lower than 50% during the measurements. Particle production was observe d on many days, typically occurring in the late morning. Under these period s of new particle production, a nucleation mode was observed to form at dia meter of the order of 3 nm and, on most occasions, this mode was observed t o grow into Aitken mode sizes over the course of a day. Total concentration s ranged from 410-45000 cm(-3), the highest concentrations occurring on par ticle production days. A clear gradient was observed between particle conce ntrations encountered below the forest canopy and those above, with signifi cantly 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 i ncreases.