Influence of water uptake on the aerosol particle light scattering coefficients of the Central European aerosol

The influence of aerosol water uptake on the aerosol particle light scattering was examined at the regional continental research site Melpitz, Germany. The scattering enhancement factor f(RH), defined as the aerosol particle scattering coefficient at a certain relative humidity (RH) divided by its d...

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Main Authors: Paul Zieger, Rahel Fierz-Schmidhauser, Laurent Poulain, Thomas Müller, Wolfram Birmili, Gerald Spindler, Alfred Wiedensohler, Urs Baltensperger, Ernest Weingartner
Format: Article
Language:English
Published: Stockholm University Press 2014-03-01
Series:Tellus: Series B, Chemical and Physical Meteorology
Subjects:
Online Access:http://www.tellusb.net/index.php/tellusb/article/download/22716/pdf_1
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author Paul Zieger
Rahel Fierz-Schmidhauser
Laurent Poulain
Thomas Müller
Wolfram Birmili
Gerald Spindler
Alfred Wiedensohler
Urs Baltensperger
Ernest Weingartner
author_facet Paul Zieger
Rahel Fierz-Schmidhauser
Laurent Poulain
Thomas Müller
Wolfram Birmili
Gerald Spindler
Alfred Wiedensohler
Urs Baltensperger
Ernest Weingartner
author_sort Paul Zieger
collection DOAJ
description The influence of aerosol water uptake on the aerosol particle light scattering was examined at the regional continental research site Melpitz, Germany. The scattering enhancement factor f(RH), defined as the aerosol particle scattering coefficient at a certain relative humidity (RH) divided by its dry value, was measured using a humidified nephelometer. The chemical composition and other microphysical properties were measured in parallel. f(RH) showed a strong variation, e.g. with values between 1.2 and 3.6 at RH=85% and λ=550 nm. The chemical composition was found to be the main factor determining the magnitude of f(RH), since the magnitude of f(RH) clearly correlated with the inorganic mass fraction measured by an aerosol mass spectrometer (AMS). Hysteresis within the recorded humidograms was observed and explained by long-range transported sea salt. A closure study using Mie theory showed the consistency of the measured parameters.
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spelling doaj.art-411d5ad955ff47f4859b2fc957b4deb62022-12-22T01:57:27ZengStockholm University PressTellus: Series B, Chemical and Physical Meteorology1600-08892014-03-0166011410.3402/tellusb.v66.2271622716Influence of water uptake on the aerosol particle light scattering coefficients of the Central European aerosolPaul Zieger0Rahel Fierz-Schmidhauser1Laurent Poulain2Thomas Müller3Wolfram Birmili4Gerald Spindler5Alfred Wiedensohler6Urs Baltensperger7Ernest Weingartner8 Paul Scherrer Institute, Laboratory of Atmospheric Chemistry, Villigen, Switzerland Paul Scherrer Institute, Laboratory of Atmospheric Chemistry, Villigen, Switzerland Leibniz Institute for Tropospheric Research, Leipzig, Germany Leibniz Institute for Tropospheric Research, Leipzig, Germany Leibniz Institute for Tropospheric Research, Leipzig, Germany Leibniz Institute for Tropospheric Research, Leipzig, Germany Leibniz Institute for Tropospheric Research, Leipzig, Germany Paul Scherrer Institute, Laboratory of Atmospheric Chemistry, Villigen, Switzerland Paul Scherrer Institute, Laboratory of Atmospheric Chemistry, Villigen, SwitzerlandThe influence of aerosol water uptake on the aerosol particle light scattering was examined at the regional continental research site Melpitz, Germany. The scattering enhancement factor f(RH), defined as the aerosol particle scattering coefficient at a certain relative humidity (RH) divided by its dry value, was measured using a humidified nephelometer. The chemical composition and other microphysical properties were measured in parallel. f(RH) showed a strong variation, e.g. with values between 1.2 and 3.6 at RH=85% and λ=550 nm. The chemical composition was found to be the main factor determining the magnitude of f(RH), since the magnitude of f(RH) clearly correlated with the inorganic mass fraction measured by an aerosol mass spectrometer (AMS). Hysteresis within the recorded humidograms was observed and explained by long-range transported sea salt. A closure study using Mie theory showed the consistency of the measured parameters.http://www.tellusb.net/index.php/tellusb/article/download/22716/pdf_1aerosol particle light scatteringhygroscopic growthscattering enhancementaerosol mass spectrometerfield measurementsoptical closure study
spellingShingle Paul Zieger
Rahel Fierz-Schmidhauser
Laurent Poulain
Thomas Müller
Wolfram Birmili
Gerald Spindler
Alfred Wiedensohler
Urs Baltensperger
Ernest Weingartner
Influence of water uptake on the aerosol particle light scattering coefficients of the Central European aerosol
Tellus: Series B, Chemical and Physical Meteorology
aerosol particle light scattering
hygroscopic growth
scattering enhancement
aerosol mass spectrometer
field measurements
optical closure study
title Influence of water uptake on the aerosol particle light scattering coefficients of the Central European aerosol
title_full Influence of water uptake on the aerosol particle light scattering coefficients of the Central European aerosol
title_fullStr Influence of water uptake on the aerosol particle light scattering coefficients of the Central European aerosol
title_full_unstemmed Influence of water uptake on the aerosol particle light scattering coefficients of the Central European aerosol
title_short Influence of water uptake on the aerosol particle light scattering coefficients of the Central European aerosol
title_sort influence of water uptake on the aerosol particle light scattering coefficients of the central european aerosol
topic aerosol particle light scattering
hygroscopic growth
scattering enhancement
aerosol mass spectrometer
field measurements
optical closure study
url http://www.tellusb.net/index.php/tellusb/article/download/22716/pdf_1
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