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Changes in submicrometer particle distributions and light scattering during haze and fog events in a highly polluted environment

Yuskiewicz, Brett A. (författare)
Leibniz Institute for Tropospheric Research (TROPOS)
Orsini, Douglas (författare)
Leibniz Institute for Tropospheric Research (TROPOS)
Stratmann, Frank (författare)
Leibniz Institute for Tropospheric Research (TROPOS)
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Wendisch, Manfred (författare)
Leibniz Institute for Tropospheric Research (TROPOS)
Wiedensohler, Alfred (författare)
Leibniz Institute for Tropospheric Research (TROPOS)
Heintzenberg, Jost (författare)
Leibniz Institute for Tropospheric Research (TROPOS)
Martinsson, Bengt G. (författare)
Lund University,Lunds universitet,Kärnfysik,Fysiska institutionen,Institutioner vid LTH,Lunds Tekniska Högskola,Nuclear physics,Department of Physics,Departments at LTH,Faculty of Engineering, LTH
Frank, Göran (författare)
Lund University,Lunds universitet,Kärnfysik,Fysiska institutionen,Institutioner vid LTH,Lunds Tekniska Högskola,Nuclear physics,Department of Physics,Departments at LTH,Faculty of Engineering, LTH
Wobrock, Wolfram (författare)
Blaise Pascal University
Schell, Dieter (författare)
Goethe University
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 (creator_code:org_t)
1998
1998
Engelska 13 s.
Ingår i: Contributions to Atmospheric Physics. - 0005-8173. ; 71:1, s. 33-45
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • The changes in submicrometer atmospheric particle size distributions measured with a Differential Mobility Particle Sizer (DMPS) system during a polluted fog experiment during November, 1994 are presented in this study. Results reveal three modes commonly evident in the size distribution (3 < DN < 843 nm) measurements; the ultrafine, Aitken and accumulation with respective geometric diameters, (Dgn), of 17, 110 and 400 nm. An additional mode, appears between the ultrafine and Aitken modes (Dgn = 52 nm) in approximately one quarter of the measurements and is linked to several industrial cities upwind of the measurement site. A stabile ultrafine mode appears consistently (84% of measurements) at 16-17 nm throughout the campaign, suggestive of a source, such as a highway in the near vicinity. During fog and haze periods number concentrations for particles less than 25 nm and greater than 400 nm decrease by 78 and 95%, respectively. These changes do not affect the aerosol scattering efficiency significantly. The overall aerosol mass scattering efficiency determined for the Po Valley region is 4.3 ± 0.6 m2 g-1. Closure is achieved for light extinction predicted from droplet distributions and measured with a transmissiometer in 37 of 39 cases during fog periods. Measured and calculated light extinction, bext, covary strongly with an R2 of 0.92.

Ämnesord

NATURVETENSKAP  -- Fysik -- Annan fysik (hsv//swe)
NATURAL SCIENCES  -- Physical Sciences -- Other Physics Topics (hsv//eng)

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