PPT-A very brief discourse on cloud microphysics

ATM 419 Spring 2016 Fovell 1 Condensed water species Cloud droplets q c Rain drops q r Ice crystals q i Snow aggregates q s Graupel particles q g Hail q. Formation of cloud droplets from supersaturated vapor. Growth of cloud droplets to raindrops in . O. (10 min). Growth of warm cloud droplets. Activated cloud droplets grow by . condensation . then . collection. - MODIS MBL Cloud Microphysics Retrievals During MAGIC and Azores IOPs Baike Xi, Xiquan Dong, Peng Wu, UND Pat Minnis , Sunny Sun - Mack, Yan Chen, NASA LaRc Acknowledgement: This research is sup rainrate. increases. Kubar. , T., D. L. Hartmann, and R. Wood, 2009: Understanding the importance of microphysics . and macrophysics . for warm rain in marine low clouds: Part I. Satellite observations. . Dr. Corey . Potvin. , CIMMS/NSSL. METR 5004 Lecture #1. Oct. 1, 2013. Preliminaries. Primarily following Wallace & Hobbs Chap. 6. Rogers & . Yau. useful as parallel text (deeper explanations). TO ENHANCED CCN CONCENTRATIONS . William R. Cotton. Department of Atmospheric Science, Colorado State University. Approaches to hailstorm simulation. 2 moment bulk microphysics. Hybrid approach: Bulk 1-M or 2-M microphysics with bin representation of hail. Presented by Lorraine A. Remer. NASA/Goddard Space Flight Center. Basis of remote sensing. Remote sensing of clouds and aerosols. Observations of aerosol modification of cloud microphysics. 3.1 Explanation. courtesy . Carly. Calvin, NCAR. NSF C-130 Platform Report. Robert Wood. (a) 20. o. S Cross-Sections [4 full missions+5. partial missions. ]. - to characterize structure of MBL, aerosols, clouds along the 20. ATM 419. Spring 2016. Fovell. 1. Definition of . “. squall line. ”. Glossary of Meteorology. (2000):. . “. a line of active thunderstorms, either continuous or with breaks, including contiguous precipitation areas resulting from the existence of thunderstorms.. Yang, M.-J., and R.A. . Houze. , . Jr. RTF. Hydrometeor types. Ice-phase microphysics. Environmental humidity. No. 1 microphysics processes. CNTL. Full model physics for 15 h. . Turn off the hail generation processes after 6 h (. ATM 419/563. Spring 2017. Fovell. 1. The C-C equation. The . Clausius-Clapeyron. (C-C) . equation reveals how saturation . vapor pressure (. e. s. ) varies . with temperature . T. :. …where . a. 1. Contributors: Chris . Bretherton. , Bill Collins, Andrew Conley, . Brian Eaton, Andrew . Gettelman. , Steve . Ghan. , . Cécile. . Hannay. , . Mike . Iacono. , . Xiaohong. Liu, Hugh Morrison, Rich Neale, . Properties: Analyses and Applications. Research Group Meeting. 10 May 2016. Scott Sieron. Advisors: . Fuqing. . Zhang, Eugene . Clothiaux. Major . Collaborator: Lu . Yinghui. COLD. WARM. Hurricane Karl 09/16/10 2315Z. cloud microphysics scheme in CAM. Hugh Morrison and Andrew . Gettelman. National Center for Atmospheric Research. CCSM Atmospheric Model Working Group Meeting. Feb 12, 2008. Thanks to Steve . Ghan. (PNNL). Hua Leighton. Collaborators: Robert Black, Frank Marks,. . . Xuejin. Zhang, . Gopal. . Sundararaman. Why do we care about microphysics?. Direct impact . . .