PPT-EXPLAIN 3. Vertical Mixing by Convection

amp Clouds EarthAtmosphere Energy Balance The air is warmed by the surface Rising thermals of air that were in direct contact with the ground Condensation of water in clouds Ideal . By Ross . Nuechterlein. Convection. Convection.  is the movement of molecules within fluids and is one of the major modes of heat and mass transfer in liquids and gas.. Buoyancy . Buoyancy.  is an upward acting force exerted by a fluid , that opposes an object's weight.. Orographic. Cumulus Clouds on the Ambient Flow. Yonggang Wang and Bart Geerts. University of Wyoming, Laramie, Wyoming, 82071, wyg@uwyo.edu. 1. Introduction. The effect of detraining cloudy air on the surrounding clear air has been studied mainly using numerical simulations. . Brian . Mapes. RSMAS. , University of Miami. Harvard, Oct 17 2009. (personal) historical moment. Two very old ideas. , . fiiinally. coming to fruition?. 1995: study convection sensitivities. inhibition vs. bulk instability (CAPE) controls. Thermohaline. Mixing in Low-Mass Red Giants. Pavel. . Denisenkov. , . UVic. 3D Numerical Simulations of . Thermohaline. Mixing in Low-Mass Red Giants. Pavel. . Denisenkov. , . UVic. A story about how important and difficult it is to take account of mixing in stars when studying stellar . AOS 453 – Spring 2014. 4/1/2014. Deep Moist Convection (. run . DMC). AOS 453 – Spring 2014. 4/1/2014. Structure Of DMC Lectures This Week. Tuesday. DMC (Convective/Convection) Initiation. Chapter 7 in MR09. GCM. convective tendencies . participate in large scale phenomena . better. Brian . Mapes. , University of Miami. trying to be CAM-useful. with much help from. Rich Neale, . Sungsu. Park, Chris . Bretherton. 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. 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 . convection scheme . in . the 5km resolution . operational system. Kengo. . Matsubayashi. . Numerical Prediction Division, . Japan . Meteorological Agency. with . Tabito. Hara, . Kohei. . Aranami. Unit B (Chapter 2). Monday 9-28-15 Starter. Is this a Vertical Stretch or Compression?. Is this a horizontal Stretch or compression?. Monday 9-28-15 Exit. Answer the following Question in sentence format.. TC. . Under . Vertical Wind Shear. . . Dandan Tao. Group meeting 09/13/2013. 1. E. xperimental. Design. WRF version 3.1. 18km, 6km, 2km; 4320km, 1440km, 720km. 41 vertical levels. ATM 419/563. Spring . 2018. Fovell. 1. The PBL. The planetary boundary layer (PBL) or atmospheric boundary layer (ABL) is the lowest part of the troposphere, where interactions with the surface are important.. Tropical . Cyclone . Lifecycle. http://glossary.ametsoc.org/wiki/Tropical_cyclone. . http://glossary.ametsoc.org/wiki/Tropical_cyclone. . TC Lifecycle Stages & Characteristics. Key structural features.