Atmos. Chem. Phys. Discuss., 10, 23091-23108, 2010
www.atmos-chem-phys-discuss.net/10/23091/2010/
doi:10.5194/acpd-10-23091-2010
© Author(s) 2010. This work is distributed
under the Creative Commons Attribution 3.0 License.
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This discussion paper has been under review for the journal Atmospheric Chemistry and Physics (ACP). Please refer to the corresponding final paper in ACP.
Influence of convection and aerosol pollution on ice cloud particle effective radius
J. H. Jiang1, H. Su1, C. Zhai1, S. T. Massie2, M. R. Schoeberl3, P. R. Colarco3, S. Platnick3, Y. Gu4, and K.-N. Liou4
1Jet propulsion Laboratory, California Institute of Technology, Pasadena, California, USA
2National Center for Atmospheric Research, Boulder, Colorado, USA
3NASA Goddard Space Flight Center, Greenbelt, Maryland, USA
4Department of Atmospheric Sciences, University of California, Los Angeles, USA

Abstract. Satellite observations show that ice cloud effective radius (re) increases with ice water content (IWC) but decreases with aerosol optical thickness (AOT). Using least-squares fitting to the observed data, we obtain an analytical formula to describe the variations of re with IWC and AOT for several regions with distinct characteristics of re-IWC-AOT relationships. As IWC directly relates to convective strength and AOT represents aerosol loading, our empirical formula provides a means to quantify the relative roles of dynamics and aerosols in controlling re in different geographical regions, and to establish a framework for parameterization of aerosol effects on re in climate models.

Citation: Jiang, J. H., Su, H., Zhai, C., Massie, S. T., Schoeberl, M. R., Colarco, P. R., Platnick, S., Gu, Y., and Liou, K.-N.: Influence of convection and aerosol pollution on ice cloud particle effective radius, Atmos. Chem. Phys. Discuss., 10, 23091-23108, doi:10.5194/acpd-10-23091-2010, 2010.
 
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