Effects of relative humidity on aerosol light scattering in the Arctic
Abstract. The effect of aerosol water uptake on the aerosol particle light scattering coefficient (σ sp ) is described in this study by comparing measurements from five European sites: the Jungfraujoch, located in the Swiss Alps at 3580 m a.s.l.; Ny-Ålesund, located on Spitsbergen in the Arctic; Mac...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.1083.5385 2023-05-15T14:53:39+02:00 Effects of relative humidity on aerosol light scattering in the Arctic P Zieger R Fierz-Schmidhauser E Weingartner U Baltensperger The Pennsylvania State University CiteSeerX Archives 2010 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1083.5385 http://www.wamis.org/agm/mumm/09-Switzerland.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1083.5385 http://www.wamis.org/agm/mumm/09-Switzerland.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.wamis.org/agm/mumm/09-Switzerland.pdf text 2010 ftciteseerx 2020-05-03T00:28:51Z Abstract. The effect of aerosol water uptake on the aerosol particle light scattering coefficient (σ sp ) is described in this study by comparing measurements from five European sites: the Jungfraujoch, located in the Swiss Alps at 3580 m a.s.l.; Ny-Ålesund, located on Spitsbergen in the Arctic; Mace Head, a coastal site in Ireland; Cabauw, a rural site in the Netherlands; and Melpitz, a regional background site in Eastern Germany. These sites were selected according to the aerosol type usually encountered at that location. The scattering enhancement factor f (RH, λ) is the key parameter to describe the effect of water uptake on the particle light scattering. It is defined as the σ sp (RH) at a certain relative humidity (RH) and wavelength λ divided by its dry value. f (RH) at the five sites varied widely, starting at very low values of f (RH = 85 %, λ = 550 nm) around 1.28 for mineral dust, and reaching up to 3.41 for Arctic aerosol. Hysteresis behavior was observed at all sites except at the Jungfraujoch (due to the absence of sea salt). Closure studies and Mie simulations showed that both size and chemical composition determine the magnitude of f (RH). Both parameters are also needed to successfully predict f (RH). Finally, the measurement results were compared to the widely used aerosol model, OPAC Text Arctic Ny Ålesund Ny-Ålesund Spitsbergen Unknown Arctic Mace ENVELOPE(155.883,155.883,-81.417,-81.417) Ny-Ålesund |
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Open Polar |
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ftciteseerx |
language |
English |
description |
Abstract. The effect of aerosol water uptake on the aerosol particle light scattering coefficient (σ sp ) is described in this study by comparing measurements from five European sites: the Jungfraujoch, located in the Swiss Alps at 3580 m a.s.l.; Ny-Ålesund, located on Spitsbergen in the Arctic; Mace Head, a coastal site in Ireland; Cabauw, a rural site in the Netherlands; and Melpitz, a regional background site in Eastern Germany. These sites were selected according to the aerosol type usually encountered at that location. The scattering enhancement factor f (RH, λ) is the key parameter to describe the effect of water uptake on the particle light scattering. It is defined as the σ sp (RH) at a certain relative humidity (RH) and wavelength λ divided by its dry value. f (RH) at the five sites varied widely, starting at very low values of f (RH = 85 %, λ = 550 nm) around 1.28 for mineral dust, and reaching up to 3.41 for Arctic aerosol. Hysteresis behavior was observed at all sites except at the Jungfraujoch (due to the absence of sea salt). Closure studies and Mie simulations showed that both size and chemical composition determine the magnitude of f (RH). Both parameters are also needed to successfully predict f (RH). Finally, the measurement results were compared to the widely used aerosol model, OPAC |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
P Zieger R Fierz-Schmidhauser E Weingartner U Baltensperger |
spellingShingle |
P Zieger R Fierz-Schmidhauser E Weingartner U Baltensperger Effects of relative humidity on aerosol light scattering in the Arctic |
author_facet |
P Zieger R Fierz-Schmidhauser E Weingartner U Baltensperger |
author_sort |
P Zieger |
title |
Effects of relative humidity on aerosol light scattering in the Arctic |
title_short |
Effects of relative humidity on aerosol light scattering in the Arctic |
title_full |
Effects of relative humidity on aerosol light scattering in the Arctic |
title_fullStr |
Effects of relative humidity on aerosol light scattering in the Arctic |
title_full_unstemmed |
Effects of relative humidity on aerosol light scattering in the Arctic |
title_sort |
effects of relative humidity on aerosol light scattering in the arctic |
publishDate |
2010 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1083.5385 http://www.wamis.org/agm/mumm/09-Switzerland.pdf |
long_lat |
ENVELOPE(155.883,155.883,-81.417,-81.417) |
geographic |
Arctic Mace Ny-Ålesund |
geographic_facet |
Arctic Mace Ny-Ålesund |
genre |
Arctic Ny Ålesund Ny-Ålesund Spitsbergen |
genre_facet |
Arctic Ny Ålesund Ny-Ålesund Spitsbergen |
op_source |
http://www.wamis.org/agm/mumm/09-Switzerland.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1083.5385 http://www.wamis.org/agm/mumm/09-Switzerland.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766325251282567168 |