Organic aerosol and global climate modelling: a review

Copernicus GmbH - Tập 5 Số 4 - Trang 1053-1123
Maria Kanakidou1, John H. Seinfeld2, Spyros Ν. Pandis3, Ian Barnes4, Frank Dentener5, M. C. Facchini6, Rita Van Dingenen5, Barbara Ervens7, Athanasios Nenes8, Claus J. Nielsen9, Erik Swietlicki10, J.-P. Putaud5, Yves Balkanski11,12, S. Fuzzi13, Jean-Claude Horth14, G. K. Moortgat15, Richard Winterhalter15, Cathrine Lund Myhre9, Kostas Tsigaridis16, E. Vignati5, Euripides G. Stephanou1, J. Wilson5
1Environmental Chemical Processes Laboratory [Heraklion]
2Departments of Chemical Engineering and Environmental Science and Engineering
3university of patras
4Bergische Universität Wuppertal
5JRC Institute for Environment and Sustainability
6Istituto di Scienze dell'Atmosfera e del Clima [Bologna]
7Institut de Chimie de Clermont-Ferrand
8School of Chemical and Biomolecular Engineering
9University of Oslo
10Skane University Hospital [Lund]
11Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette]
12Modelling the Earth Response to Multiple Anthropogenic Interactions and Dynamics
13Istituto di Scienze dell'Atmosfera e del Clima
14Climate Change Unit [Ispra]
15Max Planck Institute for Chemistry
16University of Crete [Heraklion]

Tóm tắt

Abstract. The present paper reviews existing knowledge with regard to Organic Aerosol (OA) of importance for global climate modelling and defines critical gaps needed to reduce the involved uncertainties. All pieces required for the representation of OA in a global climate model are sketched out with special attention to Secondary Organic Aerosol (SOA): The emission estimates of primary carbonaceous particles and SOA precursor gases are summarized. The up-to-date understanding of the chemical formation and transformation of condensable organic material is outlined. Knowledge on the hygroscopicity of OA and measurements of optical properties of the organic aerosol constituents are summarized. The mechanisms of interactions of OA with clouds and dry and wet removal processes parameterisations in global models are outlined. This information is synthesized to provide a continuous analysis of the flow from the emitted material to the atmosphere up to the point of the climate impact of the produced organic aerosol. The sources of uncertainties at each step of this process are highlighted as areas that require further studies.

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