Inverse modelling of cloud-aerosol interactions - Part 2: Sensitivity tests on liquid phase clouds using a Markov chain Monte Carlo based simulation approach

This paper presents a novel approach to investigate cloud-aerosol interactions by coupling a Markov chain Monte Carlo (MCMC) algorithm to an adiabatic cloud parcel model. Despite the number of numerical cloud-aerosol sensitivity studies previously conducted few have used statistical analysis tools t...

Full description

Bibliographic Details
Main Authors: Partridge, D, Vrugt, J, Tunved, P, Ekman, A, Struthers, H, Sorooshian, A
Format: Journal article
Language:English
Published: 2012
_version_ 1797062644604076032
author Partridge, D
Vrugt, J
Tunved, P
Ekman, A
Struthers, H
Sorooshian, A
author_facet Partridge, D
Vrugt, J
Tunved, P
Ekman, A
Struthers, H
Sorooshian, A
author_sort Partridge, D
collection OXFORD
description This paper presents a novel approach to investigate cloud-aerosol interactions by coupling a Markov chain Monte Carlo (MCMC) algorithm to an adiabatic cloud parcel model. Despite the number of numerical cloud-aerosol sensitivity studies previously conducted few have used statistical analysis tools to investigate the global sensitivity of a cloud model to input aerosol physiochemical parameters. Using numerically generated cloud droplet number concentration (CDNC) distributions (i.e. synthetic data) as cloud observations, this inverse modelling framework is shown to successfully estimate the correct calibration parameters, and their underlying posterior probability distribution. The employed analysis method provides a new, integrative framework to evaluate the global sensitivity of the derived CDNC distribution to the input parameters describing the lognormal properties of the accumulation mode aerosol and the particle chemistry. To a large extent, results from prior studies are confirmed, but the present study also provides some additional insights. There is a transition in relative sensitivity from very clean marine Arctic conditions where the lognormal aerosol parameters representing the accumulation mode aerosol number concentration and mean radius and are found to be most important for determining the CDNC distribution to very polluted continental environments (aerosol concentration in the accumulation mode >1000 cm-3) where particle chemistry is more important than both number concentration and size of the accumulation mode. The competition and compensation between the cloud model input parameters illustrates that if the soluble mass fraction is reduced, the aerosol number concentration, geometric standard deviation and mean radius of the accumulation mode must increase in order to achieve the same CDNC distribution. This study demonstrates that inverse modelling provides a flexible, transparent and integrative method for efficiently exploring cloud-aerosol interactions with respect to parameter sensitivity and correlation. © Author(s) 2012.
first_indexed 2024-03-06T20:48:30Z
format Journal article
id oxford-uuid:36c220b9-2f26-4545-b31e-62b68590c22f
institution University of Oxford
language English
last_indexed 2024-03-06T20:48:30Z
publishDate 2012
record_format dspace
spelling oxford-uuid:36c220b9-2f26-4545-b31e-62b68590c22f2022-03-26T13:39:53ZInverse modelling of cloud-aerosol interactions - Part 2: Sensitivity tests on liquid phase clouds using a Markov chain Monte Carlo based simulation approachJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:36c220b9-2f26-4545-b31e-62b68590c22fEnglishSymplectic Elements at Oxford2012Partridge, DVrugt, JTunved, PEkman, AStruthers, HSorooshian, AThis paper presents a novel approach to investigate cloud-aerosol interactions by coupling a Markov chain Monte Carlo (MCMC) algorithm to an adiabatic cloud parcel model. Despite the number of numerical cloud-aerosol sensitivity studies previously conducted few have used statistical analysis tools to investigate the global sensitivity of a cloud model to input aerosol physiochemical parameters. Using numerically generated cloud droplet number concentration (CDNC) distributions (i.e. synthetic data) as cloud observations, this inverse modelling framework is shown to successfully estimate the correct calibration parameters, and their underlying posterior probability distribution. The employed analysis method provides a new, integrative framework to evaluate the global sensitivity of the derived CDNC distribution to the input parameters describing the lognormal properties of the accumulation mode aerosol and the particle chemistry. To a large extent, results from prior studies are confirmed, but the present study also provides some additional insights. There is a transition in relative sensitivity from very clean marine Arctic conditions where the lognormal aerosol parameters representing the accumulation mode aerosol number concentration and mean radius and are found to be most important for determining the CDNC distribution to very polluted continental environments (aerosol concentration in the accumulation mode >1000 cm-3) where particle chemistry is more important than both number concentration and size of the accumulation mode. The competition and compensation between the cloud model input parameters illustrates that if the soluble mass fraction is reduced, the aerosol number concentration, geometric standard deviation and mean radius of the accumulation mode must increase in order to achieve the same CDNC distribution. This study demonstrates that inverse modelling provides a flexible, transparent and integrative method for efficiently exploring cloud-aerosol interactions with respect to parameter sensitivity and correlation. © Author(s) 2012.
spellingShingle Partridge, D
Vrugt, J
Tunved, P
Ekman, A
Struthers, H
Sorooshian, A
Inverse modelling of cloud-aerosol interactions - Part 2: Sensitivity tests on liquid phase clouds using a Markov chain Monte Carlo based simulation approach
title Inverse modelling of cloud-aerosol interactions - Part 2: Sensitivity tests on liquid phase clouds using a Markov chain Monte Carlo based simulation approach
title_full Inverse modelling of cloud-aerosol interactions - Part 2: Sensitivity tests on liquid phase clouds using a Markov chain Monte Carlo based simulation approach
title_fullStr Inverse modelling of cloud-aerosol interactions - Part 2: Sensitivity tests on liquid phase clouds using a Markov chain Monte Carlo based simulation approach
title_full_unstemmed Inverse modelling of cloud-aerosol interactions - Part 2: Sensitivity tests on liquid phase clouds using a Markov chain Monte Carlo based simulation approach
title_short Inverse modelling of cloud-aerosol interactions - Part 2: Sensitivity tests on liquid phase clouds using a Markov chain Monte Carlo based simulation approach
title_sort inverse modelling of cloud aerosol interactions part 2 sensitivity tests on liquid phase clouds using a markov chain monte carlo based simulation approach
work_keys_str_mv AT partridged inversemodellingofcloudaerosolinteractionspart2sensitivitytestsonliquidphasecloudsusingamarkovchainmontecarlobasedsimulationapproach
AT vrugtj inversemodellingofcloudaerosolinteractionspart2sensitivitytestsonliquidphasecloudsusingamarkovchainmontecarlobasedsimulationapproach
AT tunvedp inversemodellingofcloudaerosolinteractionspart2sensitivitytestsonliquidphasecloudsusingamarkovchainmontecarlobasedsimulationapproach
AT ekmana inversemodellingofcloudaerosolinteractionspart2sensitivitytestsonliquidphasecloudsusingamarkovchainmontecarlobasedsimulationapproach
AT struthersh inversemodellingofcloudaerosolinteractionspart2sensitivitytestsonliquidphasecloudsusingamarkovchainmontecarlobasedsimulationapproach
AT sorooshiana inversemodellingofcloudaerosolinteractionspart2sensitivitytestsonliquidphasecloudsusingamarkovchainmontecarlobasedsimulationapproach