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Microphysical modelling of aerosol scavenging by different types of clouds: description and validation of the approach
by
Hiron, Thibault
, Quérel, Arnaud
, Dépée, Alexis
, Hardy, Daniel
, Flossmann, Andrea
, Lemaitre, Pascal
, Guerra Devigne, Alice
, Monier, Marie
, Soto Minguez, Chloé
in
Aerosols
/ Analysis
/ Atmospheric and Oceanic Physics
/ Atmospheric boundary layer
/ Atmospheric transport
/ Atmospheric transport models
/ Climate models
/ Cloud formation
/ Cloud particles
/ Cloud types
/ Clouds
/ Dry deposition
/ Environmental Sciences
/ Extreme weather
/ Global climate
/ Global climate models
/ Nuclear accidents & safety
/ Ocean, Atmosphere
/ Outdoor air quality
/ Physics
/ Pollutants
/ Precipitation
/ Precipitation (Meteorology)
/ Radiation
/ Relative humidity
/ Scavenging
/ Sciences of the Universe
/ Stratus clouds
/ Transport processes
/ Weather forecasting
2024
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Microphysical modelling of aerosol scavenging by different types of clouds: description and validation of the approach
by
Hiron, Thibault
, Quérel, Arnaud
, Dépée, Alexis
, Hardy, Daniel
, Flossmann, Andrea
, Lemaitre, Pascal
, Guerra Devigne, Alice
, Monier, Marie
, Soto Minguez, Chloé
in
Aerosols
/ Analysis
/ Atmospheric and Oceanic Physics
/ Atmospheric boundary layer
/ Atmospheric transport
/ Atmospheric transport models
/ Climate models
/ Cloud formation
/ Cloud particles
/ Cloud types
/ Clouds
/ Dry deposition
/ Environmental Sciences
/ Extreme weather
/ Global climate
/ Global climate models
/ Nuclear accidents & safety
/ Ocean, Atmosphere
/ Outdoor air quality
/ Physics
/ Pollutants
/ Precipitation
/ Precipitation (Meteorology)
/ Radiation
/ Relative humidity
/ Scavenging
/ Sciences of the Universe
/ Stratus clouds
/ Transport processes
/ Weather forecasting
2024
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Microphysical modelling of aerosol scavenging by different types of clouds: description and validation of the approach
by
Hiron, Thibault
, Quérel, Arnaud
, Dépée, Alexis
, Hardy, Daniel
, Flossmann, Andrea
, Lemaitre, Pascal
, Guerra Devigne, Alice
, Monier, Marie
, Soto Minguez, Chloé
in
Aerosols
/ Analysis
/ Atmospheric and Oceanic Physics
/ Atmospheric boundary layer
/ Atmospheric transport
/ Atmospheric transport models
/ Climate models
/ Cloud formation
/ Cloud particles
/ Cloud types
/ Clouds
/ Dry deposition
/ Environmental Sciences
/ Extreme weather
/ Global climate
/ Global climate models
/ Nuclear accidents & safety
/ Ocean, Atmosphere
/ Outdoor air quality
/ Physics
/ Pollutants
/ Precipitation
/ Precipitation (Meteorology)
/ Radiation
/ Relative humidity
/ Scavenging
/ Sciences of the Universe
/ Stratus clouds
/ Transport processes
/ Weather forecasting
2024
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Microphysical modelling of aerosol scavenging by different types of clouds: description and validation of the approach
Journal Article
Microphysical modelling of aerosol scavenging by different types of clouds: description and validation of the approach
2024
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Overview
With dry deposition and below-cloud scavenging, in-cloud scavenging is one of the three components of aerosol transfer from the atmosphere to the ground. There is no experimental validation of in-cloud particle scavenging models for all cloud types that is not impacted by uncertainties concerning below-cloud scavenging. In this article, the choice was made to start with a recognised and validated microphysical cloud formation model (the DEtailed SCAvenging Model, DESCAM) to extract a scheme of aerosol scavenging by clouds, valid for different cloud types. The resulting model works for the two most extreme precipitation clouds: from cumulonimbus to stratus. It is based on data accessible a priori from numerical weather prediction (NWP) outputs, i.e. the intensity of the rain and the relative humidity in the cloud. The diagnostic of the altitude of the cloud base proves to be a key parameter, and accuracy in this regard is vital. This new in-cloud scavenging scheme is intended for use in long-distance (> 100 km) atmospheric transport models (ATMs) or global climate models (GCMs).
Publisher
Copernicus GmbH,European Geosciences Union,Copernicus Publications
Subject
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