![]() ![]() ![]() 1990) Hard to measure Shattering of large particles Gardiner and Hallett 1985 Gayet et al. 1988 Jensen et al ) Cloud feedback (e.g., Stephens et al. In-situ measurements Scattering model microphysics GCMs Ice Particle Model Satellite remote sensingħ Ice particle model Size distribution Shape distribution OrientationĬloud life time (e.g., Heymsfield 1972, Jensen et al.1996) Cloud reflectance, radiative forcing, heating/cooling rate (e.g., Ackerman et al. Ice clouds are important, because Cover large portion of the Earth’s surface Radiative effects Water vapor budget Cloud feedbacks ISCCP day-time ice cloud amount Earth Albedo Effect Greenhouse Effect (dominant)Ħ Satellite-base remote sensing of ice cloud properties Importance of ice cloud Ice particle model and ice cloud retrieval Influence of ice particle model on t retrieval Comparison of MODIS and POLDER ice t retrieval Influence on our understanding of ice cloud seasonal variability SummaryĤ Ice cloud: important ISCCP day-time ice cloud amount Albedo Effect Influences of ice particle model on ice cloud optical thickness retrieval Zhibo (zippo) Zhang ESSICĢ Outline Background Influence of ice particle model on t retrieval
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