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Statistical characterization of air ion mobility spectra at Tahkuse Observatory: Classification of air ions
Author(s) -
Hõrrak U.,
Salm J.,
Tammet H.
Publication year - 2000
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/1999jd901197
Subject(s) - ion , aerosol , spectral line , range (aeronautics) , cluster (spacecraft) , observatory , analytical chemistry (journal) , physics , materials science , astrophysics , chemistry , meteorology , astronomy , chromatography , quantum mechanics , computer science , composite material , programming language
A database of 8615 hourly averaged air ion mobility spectra in the range of 0.00041–3.2 cm 2 V −1 s −1 was measured at Tahkuse Observatory, Estonia, during 14 months in 1993–1994. The average mobility spectrum over the whole period shows distinct peaks of small and large ions. Intermediate ions with mobilities of 0.034–0.5 cm 2 V −1 s −1 are of low concentration of about 50 cm −3 in the average spectrum. They experience occasional bursts of up to about 900 cm −3 during 6–10 hours at daytime. The number of burst events recorded during 14 months was 101, with maximum frequency in spring and minimum frequency in winter. Physically, large and intermediate ions can be called aerosol ions, and small ions can be called cluster ions. The principal component analysis was applied to detect the structure of an air ion mobility spectrum. As a result, the mobility spectrum in the range of 0.00041–3.2 cm 2 V −1 s −1 (diameters of 0.36–79 nm) was divided into five classes: small cluster, big cluster, intermediate, light large, and heavy large ions. The boundaries between the classes are 1.3 cm 2 V −1 s −1 (diameter of 0.85 nm), 0.5 cm 2 V −1 s −1 (1.6 nm), 0.034 cm 2 V −1 s −1 (7.4 nm), and 0.0042 cm 2 V −1 s −1 (22 nm). The five principal components that are closely correlated with the respective ion classes explain 92% of total variance. The classification of aerosol ions is in accord with the three‐modal structure of the size spectrum of submicron aerosol particles.

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