AerSett v1.0: a simple and straightforward model for the settling speed of big spherical atmospheric aerosols

<p>This study introduces AerSett v1.0 (AERosol SETTling version 1.0), a model giving the settling speed of big spherical aerosols in the atmosphere without going through an iterative equation resolution. We prove that, for all spherical atmospheric aerosols with diameter <span class="i...

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Main Authors: S. Mailler, L. Menut, A. Cholakian, R. Pennel
Format: Article
Language:English
Published: Copernicus Publications 2023-02-01
Series:Geoscientific Model Development
Online Access:https://gmd.copernicus.org/articles/16/1119/2023/gmd-16-1119-2023.pdf
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author S. Mailler
S. Mailler
L. Menut
A. Cholakian
R. Pennel
author_facet S. Mailler
S. Mailler
L. Menut
A. Cholakian
R. Pennel
author_sort S. Mailler
collection DOAJ
description <p>This study introduces AerSett v1.0 (AERosol SETTling version 1.0), a model giving the settling speed of big spherical aerosols in the atmosphere without going through an iterative equation resolution. We prove that, for all spherical atmospheric aerosols with diameter <span class="inline-formula"><i>D</i></span> up to <span class="inline-formula">1000 µm</span>, this direct and explicit method including the drag coefficient formulation of <span class="cit" id="xref_text.1"><a href="#bib1.bibx5">Clift and Gauvin</a> (<a href="#bib1.bibx5">1971</a>)</span> and the <span class="cit" id="xref_text.2"><a href="#bib1.bibx7">Davies</a> (<a href="#bib1.bibx7">1945</a>)</span> slip correction factor gives results within 2 % of the exact solution obtained from the numerical resolution of a non-linear fixed-point equation. This error is acceptable considering the uncertainties on the drag coefficient formulations themselves. For <span class="inline-formula"><i>D</i>&lt;100 µm</span>, the error is below 0.5 %. We provide a Fortran implementation of this simple and straightforward model, hoping that more chemistry–transport models (CTMs) and general circulation models will be able to take into account large-particle drag correction to the settling speed of big spherical aerosol particles in the atmosphere, without performing an iterative and time-consuming calculation.</p>
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spelling doaj.art-d9f587fd89604aa3a7c9be7a0ff267942023-02-15T07:46:11ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032023-02-01161119112710.5194/gmd-16-1119-2023AerSett v1.0: a simple and straightforward model for the settling speed of big spherical atmospheric aerosolsS. Mailler0S. Mailler1L. Menut2A. Cholakian3R. Pennel4LMD/IPSL, École Polytechnique, Institut Polytechnique de Paris, ENS, PSL Research University, Sorbonne Université, CNRS, Palaiseau, FranceÉcole des Ponts ParisTech, Marne-la-Vallée, FranceLMD/IPSL, École Polytechnique, Institut Polytechnique de Paris, ENS, PSL Research University, Sorbonne Université, CNRS, Palaiseau, FranceLMD/IPSL, École Polytechnique, Institut Polytechnique de Paris, ENS, PSL Research University, Sorbonne Université, CNRS, Palaiseau, FranceLMD/IPSL, École Polytechnique, Institut Polytechnique de Paris, ENS, PSL Research University, Sorbonne Université, CNRS, Palaiseau, France<p>This study introduces AerSett v1.0 (AERosol SETTling version 1.0), a model giving the settling speed of big spherical aerosols in the atmosphere without going through an iterative equation resolution. We prove that, for all spherical atmospheric aerosols with diameter <span class="inline-formula"><i>D</i></span> up to <span class="inline-formula">1000 µm</span>, this direct and explicit method including the drag coefficient formulation of <span class="cit" id="xref_text.1"><a href="#bib1.bibx5">Clift and Gauvin</a> (<a href="#bib1.bibx5">1971</a>)</span> and the <span class="cit" id="xref_text.2"><a href="#bib1.bibx7">Davies</a> (<a href="#bib1.bibx7">1945</a>)</span> slip correction factor gives results within 2 % of the exact solution obtained from the numerical resolution of a non-linear fixed-point equation. This error is acceptable considering the uncertainties on the drag coefficient formulations themselves. For <span class="inline-formula"><i>D</i>&lt;100 µm</span>, the error is below 0.5 %. We provide a Fortran implementation of this simple and straightforward model, hoping that more chemistry–transport models (CTMs) and general circulation models will be able to take into account large-particle drag correction to the settling speed of big spherical aerosol particles in the atmosphere, without performing an iterative and time-consuming calculation.</p>https://gmd.copernicus.org/articles/16/1119/2023/gmd-16-1119-2023.pdf
spellingShingle S. Mailler
S. Mailler
L. Menut
A. Cholakian
R. Pennel
AerSett v1.0: a simple and straightforward model for the settling speed of big spherical atmospheric aerosols
Geoscientific Model Development
title AerSett v1.0: a simple and straightforward model for the settling speed of big spherical atmospheric aerosols
title_full AerSett v1.0: a simple and straightforward model for the settling speed of big spherical atmospheric aerosols
title_fullStr AerSett v1.0: a simple and straightforward model for the settling speed of big spherical atmospheric aerosols
title_full_unstemmed AerSett v1.0: a simple and straightforward model for the settling speed of big spherical atmospheric aerosols
title_short AerSett v1.0: a simple and straightforward model for the settling speed of big spherical atmospheric aerosols
title_sort aersett v1 0 a simple and straightforward model for the settling speed of big spherical atmospheric aerosols
url https://gmd.copernicus.org/articles/16/1119/2023/gmd-16-1119-2023.pdf
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