Apparatus for dry deposition of aerosols on snow

<p>Deposition of light-absorbing aerosol on snow can drastically change the albedo of the snow surface and the energy balance of the snowpack. To study these important effects experimentally and to compare them with theory, it is desirable to have an apparatus for such deposition experiments....

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Main Authors: N. D. Beres, H. Moosmüller
Format: Article
Language:English
Published: Copernicus Publications 2018-12-01
Series:Atmospheric Measurement Techniques
Online Access:https://www.atmos-meas-tech.net/11/6803/2018/amt-11-6803-2018.pdf
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spelling doaj-4a51376a74f44eb4a028ec8e02d009212020-11-24T20:57:00ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482018-12-01116803681310.5194/amt-11-6803-2018Apparatus for dry deposition of aerosols on snowN. D. Beres0N. D. Beres1H. Moosmüller2Laboratory for Aerosol Science, Spectroscopy, and Optics, Desert Research Institute, Reno, NV 89512, USADepartment of Physics, University of Nevada–Reno, Reno, NV 89512, USALaboratory for Aerosol Science, Spectroscopy, and Optics, Desert Research Institute, Reno, NV 89512, USA<p>Deposition of light-absorbing aerosol on snow can drastically change the albedo of the snow surface and the energy balance of the snowpack. To study these important effects experimentally and to compare them with theory, it is desirable to have an apparatus for such deposition experiments. Here, we describe a simple apparatus to generate and evenly deposit light-absorbing aerosols onto a flat snow surface. Aerosols are produced (combustion aerosols) or entrained (mineral dust aerosols) and continuously transported into a deposition chamber placed on the snow surface where they deposit onto and into the snowpack, thereby modifying its surface reflectance and albedo. We demonstrate field operation of this apparatus by generating black and brown carbon combustion aerosols and entraining hematite mineral dust aerosol and depositing them on the snowpack. Changes in spectral snow reflectance are demonstrated qualitatively through pictures of snow surfaces after aerosol deposition and quantitatively by measuring hemispherical-conical reflectance spectra for the deposited areas and for adjacent snowpack in its natural state. Additional potential applications for this apparatus are mentioned and briefly discussed.</p>https://www.atmos-meas-tech.net/11/6803/2018/amt-11-6803-2018.pdf
collection DOAJ
language English
format Article
sources DOAJ
author N. D. Beres
N. D. Beres
H. Moosmüller
spellingShingle N. D. Beres
N. D. Beres
H. Moosmüller
Apparatus for dry deposition of aerosols on snow
Atmospheric Measurement Techniques
author_facet N. D. Beres
N. D. Beres
H. Moosmüller
author_sort N. D. Beres
title Apparatus for dry deposition of aerosols on snow
title_short Apparatus for dry deposition of aerosols on snow
title_full Apparatus for dry deposition of aerosols on snow
title_fullStr Apparatus for dry deposition of aerosols on snow
title_full_unstemmed Apparatus for dry deposition of aerosols on snow
title_sort apparatus for dry deposition of aerosols on snow
publisher Copernicus Publications
series Atmospheric Measurement Techniques
issn 1867-1381
1867-8548
publishDate 2018-12-01
description <p>Deposition of light-absorbing aerosol on snow can drastically change the albedo of the snow surface and the energy balance of the snowpack. To study these important effects experimentally and to compare them with theory, it is desirable to have an apparatus for such deposition experiments. Here, we describe a simple apparatus to generate and evenly deposit light-absorbing aerosols onto a flat snow surface. Aerosols are produced (combustion aerosols) or entrained (mineral dust aerosols) and continuously transported into a deposition chamber placed on the snow surface where they deposit onto and into the snowpack, thereby modifying its surface reflectance and albedo. We demonstrate field operation of this apparatus by generating black and brown carbon combustion aerosols and entraining hematite mineral dust aerosol and depositing them on the snowpack. Changes in spectral snow reflectance are demonstrated qualitatively through pictures of snow surfaces after aerosol deposition and quantitatively by measuring hemispherical-conical reflectance spectra for the deposited areas and for adjacent snowpack in its natural state. Additional potential applications for this apparatus are mentioned and briefly discussed.</p>
url https://www.atmos-meas-tech.net/11/6803/2018/amt-11-6803-2018.pdf
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