PPT-Convective and stratiform microphysics and dynamics

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Courtney Schumacher for Brians mesoscale class First tropical radar bright band Murty et al 1965 African squall line evolution Chong et al 1987 African squall line

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Convective and stratiform microphysics and dynamics: Transcript


Courtney Schumacher for Brians mesoscale class First tropical radar bright band Murty et al 1965 African squall line evolution Chong et al 1987 African squall line mature stage Chong et al 1987. Robert A. Houze, Jr.. University of Washington. ISSCP at 30, New York, 22 April 2013. Radars in Space. CloudSat. 2006-. TRMM. 1997-. Epic Floods . in . Pakistan. 2010, 2011, 2012. 25N. 30N. 65. E. 7. Hannah C. Barnes. Robert A. Houze, Jr.. University of Washington. 31. st. Conference on Hurricanes and Tropical Meteorology . Town & Country Resort and Conference Center, San Diego, CA. 2 April 2014. Hannah C. Barnes. Robert A. Houze, Jr.. University of Washington. Presentation by H. Barnes at Department of Meteorology, . The Pennsylvania . State University, State . Callege. , PA, August 15, 2014. Limitations. R. Houze. University of Washington. CaPPM. Meeting, JPL, Pasadena, October 1, 2014. TRMM. GPM. CloudSat .  . EarthCare. TRMM and CloudSat analyses in the tropics: Advantages and . Crystal K Williams. Department of Geography-Geology. Illinois State University. Outline. Introduction/Background. Mesoscale Convective Systems. Squall Lines. Precipitation. Conclusions. Introduction. Challenges for the Next Decades. NASA Earth Science Division Workshop, NASA/Ames, 6-8 May 2014. Robert A. Houze, Jr.. University of Washington. Fair weather cumulus. Cumulus congestus. Cumulonimbus. Single cell. Loosely defined: A line of either ordinary cells or supercells of finite length (10- hundreds of km) that may contain a stratiform rain region either behind, parallel to, or ahead of the convective line.. Microphysics droplet concentration. 5. Conclusions. The sea ice state simulated in RASM is sensitive to the details of the WRF radiation and microphysics treatment, with coupling between the radiation and microphysics parameterization resulting in improved sea ice simulation (Figure 4).. Weather Systems – Fall 2015. Outline:. a. Stability Indices. b. Wind Shear and . Helicity. c. How to relate to predicted / observed convective weather. Convective Parameters. Weather Systems – Fall 2015. Atmos. Sci. Colloquium, Seattle, 6 April 2012. R. Houze. and. . D. Hence, S. . Brodzik. , K. Rasmussen, S. Powell, H. Barnes, . B. Dolan, K. . Chakravarty. , C. . Burleyson. , Z. Li,. S. Ellis, T. . &. related issues. P. . Mukhopadhyay. Climate v. Numerical Weather Prediction. NWP: . Initial state is CRITICAL. Don’t really care about whole PDF, just probable phase space. conservation of mass/energy to match observed state. 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). 2. from TOGA COARE*. Richard H. Johnson . Paul E. . Ciesielski. Colorado State University. Thomas M. . Rickenbach. East Carolina University. * . D. edicated to . Michio. . Yanai. (AMS Monograph). Yanai. Kerry Emanuel. Massachusetts Institute of Technology. Several Possibly Inter-related Enigmas of the Tropical Atmosphere. Why does moist convection often cluster?. What determines the number of tropical cyclones on the planet?.

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