Wildfires as a source of airborne mineral dust – revisiting a conceptual model using large-eddy simulation (LES)

<p>Airborne mineral dust is a key player in the Earth system and shows manifold impacts on atmospheric properties such as the radiation budget and cloud microphysics. Investigations of smoke plumes originating from wildfires found significant fractions of mineral dust within these plumes –...

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Main Authors: R. Wagner, M. Jähn, K. Schepanski
Format: Article
Language:English
Published: Copernicus Publications 2018-08-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/18/11863/2018/acp-18-11863-2018.pdf
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author R. Wagner
M. Jähn
M. Jähn
K. Schepanski
author_facet R. Wagner
M. Jähn
M. Jähn
K. Schepanski
author_sort R. Wagner
collection DOAJ
description <p>Airborne mineral dust is a key player in the Earth system and shows manifold impacts on atmospheric properties such as the radiation budget and cloud microphysics. Investigations of smoke plumes originating from wildfires found significant fractions of mineral dust within these plumes – most likely raised by strong, turbulent fire-related winds. This study presents and revisits a conceptual model describing the emission of mineral dust particles during wildfires. This is achieved by means of high-resolution large-eddy simulation (LES), conducted with the All Scale Atmospheric Model (ASAM). The impact of (a) different fire properties representing idealized grassland and shrubland fires, (b) different ambient wind conditions modulated by the fire's energy flux, and (c) the wind's capability to mobilize mineral dust particles was investigated. Results from this study illustrate that the energy release of the fire leads to a significant increase in near-surface wind speed, which consequently enhances the dust uplift potential. This is in particular the case within the fire area where vegetation can be assumed to be widely removed and uncovered soil is prone to wind erosion. The dust uplift potential is very sensitive to fire properties, such as fire size, shape, and intensity, but also depends on the ambient wind velocity. Although measurements already showed the importance of wildfires for dust emissions, pyro-convection is so far neglected as a dust emission process in atmosphere–aerosol models. The results presented in this study can be seen as the first step towards a systematic parameterization representing the connection between typical fire properties and related dust emissions.</p>
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spelling doaj.art-4b1ca66d0ada40ceafc7681cc58c8acf2022-12-21T18:55:08ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242018-08-0118118631188410.5194/acp-18-11863-2018Wildfires as a source of airborne mineral dust – revisiting a conceptual model using large-eddy simulation (LES)R. Wagner0M. Jähn1M. Jähn2K. Schepanski3Leibniz Institute for Tropospheric Research (TROPOS), Leipzig, GermanyLeibniz Institute for Tropospheric Research (TROPOS), Leipzig, Germanynow at: Swiss Federal Laboratories for Material Science and Technology (Empa), Dübendorf, SwitzerlandLeibniz Institute for Tropospheric Research (TROPOS), Leipzig, Germany<p>Airborne mineral dust is a key player in the Earth system and shows manifold impacts on atmospheric properties such as the radiation budget and cloud microphysics. Investigations of smoke plumes originating from wildfires found significant fractions of mineral dust within these plumes – most likely raised by strong, turbulent fire-related winds. This study presents and revisits a conceptual model describing the emission of mineral dust particles during wildfires. This is achieved by means of high-resolution large-eddy simulation (LES), conducted with the All Scale Atmospheric Model (ASAM). The impact of (a) different fire properties representing idealized grassland and shrubland fires, (b) different ambient wind conditions modulated by the fire's energy flux, and (c) the wind's capability to mobilize mineral dust particles was investigated. Results from this study illustrate that the energy release of the fire leads to a significant increase in near-surface wind speed, which consequently enhances the dust uplift potential. This is in particular the case within the fire area where vegetation can be assumed to be widely removed and uncovered soil is prone to wind erosion. The dust uplift potential is very sensitive to fire properties, such as fire size, shape, and intensity, but also depends on the ambient wind velocity. Although measurements already showed the importance of wildfires for dust emissions, pyro-convection is so far neglected as a dust emission process in atmosphere–aerosol models. The results presented in this study can be seen as the first step towards a systematic parameterization representing the connection between typical fire properties and related dust emissions.</p>https://www.atmos-chem-phys.net/18/11863/2018/acp-18-11863-2018.pdf
spellingShingle R. Wagner
M. Jähn
M. Jähn
K. Schepanski
Wildfires as a source of airborne mineral dust – revisiting a conceptual model using large-eddy simulation (LES)
Atmospheric Chemistry and Physics
title Wildfires as a source of airborne mineral dust – revisiting a conceptual model using large-eddy simulation (LES)
title_full Wildfires as a source of airborne mineral dust – revisiting a conceptual model using large-eddy simulation (LES)
title_fullStr Wildfires as a source of airborne mineral dust – revisiting a conceptual model using large-eddy simulation (LES)
title_full_unstemmed Wildfires as a source of airborne mineral dust – revisiting a conceptual model using large-eddy simulation (LES)
title_short Wildfires as a source of airborne mineral dust – revisiting a conceptual model using large-eddy simulation (LES)
title_sort wildfires as a source of airborne mineral dust revisiting a conceptual model using large eddy simulation les
url https://www.atmos-chem-phys.net/18/11863/2018/acp-18-11863-2018.pdf
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