PPT-Multisensor Investigation of Deep Convection

AGU San Francisco 5 December 2012 Robert A Houze Jr amp Jian Yuan University of Washington Mesoscale Convective Systems MCSs Large areas of cold top Example outbreak of MCSs. atmospheric convection. Brian Mapes. Rosenstiel School of Marine and Atmospheric Sciences, U. of Miami. with. Zhiming Kuang, Harvard University. Physical importance of convection. v. ertical flux of . David M. Romps. Workshop on Large-Scale Circulations. in Moist Convecting Atmospheres. October. 17, 2009. The bulk. -plume equations. , when used to diagnose large-eddy simulations, underestimate convective entrainment.. Brian Mapes, U of Miami. with. Baohua Chen (UM). Richard Neale (NCAR). Emily Riley (UM). Organ-ization. From Greek organon. about . instrumentality . or . working order. "Organized" convection. (weak) Something is making it patterned . boundary . layer and . orographic. circulation . with . locally-triggered deep convection around the Santa Catalina Mountains in Arizona. Bart Geerts . (geerts@uwyo.edu) . . J. Robert A. Houze, Jr.. University of Washington. with: K. L. Rasmussen, M. D. Zuluaga, and S. R. Brodzik. European Geosciences Union General Assembly, Vienna, Austria 17 April 2015 . The TRMM Satellite. Part 2 – Modes of Isolated Organization. AOS 453 – Spring 2014. 4/3/. 2014. Structure Of DMC Lectures This Week. Tuesday. DMC (Convective/Convection) Initiation. Chapter 7 in MR09. Isolated DMC Organization (Part 1). &. 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. Robert A. Houze, Jr.. University of Washington. with: K. L. Rasmussen, M. D. Zuluaga, and S. R. Brodzik. Presented at:. AGU Fall Meeting, San Francisco, 18 December 2015 . The TRMM Satellite. 1997-2014. deep, moist convection. Bogdan Antonescu. University of Manchester. (some slides courtesy of C. . Doswell. ). Mesoscale. Ingredients for deep, moist convection. Instability. . – conditional instability: (lapse rate) needed to develop . effects of terrain on . precipitation. The wind began to blow steadily out of the west and pour the water of the distant seas on the dark heads of the hills . … . J.R.R. Tolkien, The Lord of the Rings. EMC/NCEP/NWS/NOAA. Young C. Kwon, V. Tallapragada, R. Tuleya, Q. Liu, K. Yeh*, S. Gopal*, Z. Zhang, S. Trahan and J. O’connor . *: HRD/AOML. Use WRF-NMM3.2 . dynamic core. . Upgrade the . vortex initialization. of the UM in different parts of the world.. Humphrey Lean, Kirsty Hanley, Stuart Webster, Will Keat, Thorwald Stein, Todd Lane, Martin Jucker, Elizabeth Kendon and Giorgia Fosser. Met Office has run 1.5km UK version of Unified Model for about 10 years (UKV). . Why is it windy at the seaside?. Cold air sinks. Where is the freezer compartment put in a fridge?. Freezer compartment. It is put at the top, because cool air sinks, so it cools the food on the way down.. 2. nd. PAZ Polarimetric Radio Occultations User Workshop. Terence Kubar. 2,1. Manuel de la Torre Ju. rez. 1. Jonas Katona. 1. . F. Joseph Turk. 1. . Ramon . Padull. s. 3,4.  . 1. Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA.