http://www.cnr.it/ontology/cnr/individuo/prodotto/ID44741
The effect of physical and chemical aerosol properties on warm cloud droplet activation. (Articolo in rivista)
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- Label
- The effect of physical and chemical aerosol properties on warm cloud droplet activation. (Articolo in rivista) (literal)
- Anno
- 2006-01-01T00:00:00+01:00 (literal)
- Alternative label
McFiggans, G., P. Artaxo, U. Baltensperger, H. Coe, M.C. Facchini, G. Feingold, S. Fuzzi, M. Gysel, A. Laaksonen, U. Lohmann, T.F. Mentel, D.M. Murphy, C.D. O'Dowd, J. R. Snider and E. Weingartner (2006)
The effect of physical and chemical aerosol properties on warm cloud droplet activation.
in Atmospheric chemistry and physics (Online)
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- McFiggans, G., P. Artaxo, U. Baltensperger, H. Coe, M.C. Facchini, G. Feingold, S. Fuzzi, M. Gysel, A. Laaksonen, U. Lohmann, T.F. Mentel, D.M. Murphy, C.D. O'Dowd, J. R. Snider and E. Weingartner (literal)
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- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Univ Manchester, SEAES, Atmospher Sci Grp, Manchester M60 1QD, Lancs, England
Univ Sao Paulo, Inst Fis, BR-05508900 Sao Paulo, Brazil
Paul Scherrer Inst, Lab Atmospharenchem, CH-5232 Villigen, Switzerland
CNR, Ist Sci Atmosfera & Clima, I-40129 Bologna, Italy
NOAA, Environm Technol Lab, Boulder, CO 80305 USA
Univ Kuopio, Dept Appl Phys, FIN-70211 Kuopio, Finland
ETH, Inst Atmospher & Climate Sci, CH-8093 Zurich, Switzerland
Forschungszentrum Julich, ICG Troposphare 2, D-52425 Julich, Germany
NOAA, Aeron Lab, Boulder, CO 80305 USA
Natl Univ Ireland, Dept Phys, Galway, Ireland
Univ Wyoming, Dept Atmospher Sci, Laramie, WY 82071 USA (literal)
- Titolo
- The effect of physical and chemical aerosol properties on warm cloud droplet activation. (literal)
- Abstract
- The effects of atmospheric aerosol on climate forcing may be very substantial but are quantified poorly at present; in particular, the effects of aerosols on cloud radia-tive properties, or the indirect effects are credited with the greatest range of uncertainty amongst the known causes of radiative forcing. This manuscript explores the effects that the composition and properties of atmospheric aerosol can have on the activation of droplets in warm clouds, so poten-tially influencing the magnitude of the indirect effect. The effects of size, composition, mixing state and various derived properties are assessed and a range of these properties pro-vided by atmospheric measurements in a variety of locations is briefly reviewed. The suitability of a range of process-level descriptions to capture these aerosol effects is investigated by assessment of their sensitivities to uncertainties in aerosol properties and by their performance in closure studies. The treatment of these effects within global models is reviewed and suggestions for future investigations are made. (literal)
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