PPT-Relating Large-Scale Vertical Motions to MJO Convective Ons

Scott W Powell and Robert A Houze Jr University of Washington Seattle WA 1 Introduction Work on this poster was supported by DOE grant DE SC0008452 NSF grants AGS1059611 and AGS1355567 and NASA grants NNX10AH70G and NNX13AG71G. By. Chi . Bemieh. . Fule. August 6, 2013. THESIS PRESENTATION . Outline. . of. . today’s. presentation. Justification of the study. Problem . statement. Hypotheses. Conceptual. . framework. Research . 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 . Achatz. Goethe-. Universität. Frankfurt am Main. Multiple-scale . asymptotics. . of the interaction between. gravity waves and synoptic-scale flow. and its implications for. soundproof . modelling. Gregory . Falkovich. Weizmann Institute of Science, Israel. April 01, 2013, Berkeley. “The answer is blowing in the wind”. Only normal forces. S. S’. Horizontal temperature . gradient causes wind. 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. MODIS. , TRMM, and ECMWF-Interim Reanalysis Data. TERRA/AQUA PI: . Terry Kubar (UCLA/JIFRESSE). Co-I: . Ali . Behrangi. (JPL). Collaborator: . Graeme Stephens (JPL). MODIS Science Team Meeting – Atmosphere Team Breakout Session. &. 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. Oscillations . . 伴隨季內震盪的. 雲. 水. 過程. 分析. Chung-. Hsiung. Sui . Dept. of Atmospheric Sciences . National Taiwan . University. 隋中興 洪竟書. . 曾開智. . 台灣大學大氣科學系. Robert A. Houze, Jr.. With contributions from:. S. Powell, M. . Zuluaga. , H. Barnes, A. Rowe. AGU Annual Meeting, San Francisco, 11 December 2013. The MJO scale. ~30-60 days. TOGA. COARE. West Pacific. Luke Madaus – 27 May 2016. PhD Defense – University of Washington. Where this all began. Where this all began. …others were thinking about this too. Predicting discrete convective initiation (CI) is a. MODIS. , TRMM, and ECMWF-Interim Reanalysis Data. TERRA/AQUA PI: . Terry Kubar (UCLA/JIFRESSE). Co-I: . Ali . Behrangi. (JPL). Collaborator: . Graeme Stephens (JPL). MODIS Science Team Meeting – Atmosphere Team Breakout Session. Workshop on the Tropical Dynamics and the MJO, . Honolulu, January 14-15 2014. Understanding of essential dynamics of the MJO. MJO. –. a Dynamic Definition . An equatorial . planetary scale . circulation system coupled with a . & its relation with trace gas transport. ATTREX/CONTRAST/CAST Science Team Meeting, Oct, 2014 . Ji-Eun Kim. University of Colorado, Boulder, CO. M. Joan Alexander. NWRA/Colorado Research Associates, Boulder, CO. Yaxin Li and Prof. Sally M. Benson. Department of Energy Resources Engineering. Stanford University. Nov 9. th. , 2021. The long-term fate of residually trapped gas is unclear. In CO. 2. storage, a large fraction of injected gas is residually trapped in pore spaces by capillary forces..