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Global analysis of continental boundary layer new particle formation based on long-term measurements

Authors :
T. Nieminen
V.-M. Kerminen
T. Petäjä
P. P. Aalto
M. Arshinov
E. Asmi
U. Baltensperger
D. C. S. Beddows
J. P. Beukes
D. Collins
A. Ding
R. M. Harrison
B. Henzing
R. Hooda
M. Hu
U. Hõrrak
N. Kivekäs
K. Komsaare
R. Krejci
A. Kristensson
L. Laakso
A. Laaksonen
W. R. Leaitch
H. Lihavainen
N. Mihalopoulos
Z. Németh
W. Nie
C. O'Dowd
I. Salma
K. Sellegri
B. Svenningsson
E. Swietlicki
P. Tunved
V. Ulevicius
V. Vakkari
M. Vana
A. Wiedensohler
Z. Wu
A. Virtanen
M. Kulmala
Source :
Atmospheric Chemistry and Physics, Vol 18, Pp 14737-14756 (2018)
Publication Year :
2018
Publisher :
Copernicus Publications, 2018.

Abstract

Atmospheric new particle formation (NPF) is an important phenomenon in terms of global particle number concentrations. Here we investigated the frequency of NPF, formation rates of 10 nm particles, and growth rates in the size range of 10–25 nm using at least 1 year of aerosol number size-distribution observations at 36 different locations around the world. The majority of these measurement sites are in the Northern Hemisphere. We found that the NPF frequency has a strong seasonal variability. At the measurement sites analyzed in this study, NPF occurs most frequently in March–May (on about 30 % of the days) and least frequently in December–February (about 10 % of the days). The median formation rate of 10 nm particles varies by about 3 orders of magnitude (0.01–10 cm−3 s−1) and the growth rate by about an order of magnitude (1–10 nm h−1). The smallest values of both formation and growth rates were observed at polar sites and the largest ones in urban environments or anthropogenically influenced rural sites. The correlation between the NPF event frequency and the particle formation and growth rate was at best moderate among the different measurement sites, as well as among the sites belonging to a certain environmental regime. For a better understanding of atmospheric NPF and its regional importance, we would need more observational data from different urban areas in practically all parts of the world, from additional remote and rural locations in North America, Asia, and most of the Southern Hemisphere (especially Australia), from polar areas, and from at least a few locations over the oceans.

Subjects

Subjects :
Physics
QC1-999
Chemistry
QD1-999

Details

Language :
English
ISSN :
16807316 and 16807324
Volume :
18
Database :
Directory of Open Access Journals
Journal :
Atmospheric Chemistry and Physics
Publication Type :
Academic Journal
Accession number :
edsdoj.4f9a1a7b47ee421d8b2b270d59fdfb0b
Document Type :
article
Full Text :
https://doi.org/10.5194/acp-18-14737-2018