PPT-Chapter 4. Convective Dynamics

46 Supercell Storms Photographs   Todd Lindley                                                                                                  . Robert A. Houze, Jr.. University of Washington. ASR Science Team Meetings, Bethesda, 20 November 2014 . Mesoscale Convective Systems. 1. 2. 3. From space. Frequency of MCS anvils over tropics. Yuan and Houze 2010. Convective Dynamics. 4.5. Bright Bands, Bow Echoes and Mesoscale Convective Complexes. Photographs ©  Todd Lindley. . Bright band associated with stratiform precipitation in a squall line system. Bright band associated with stratiform precipitation. 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. Fig. 3: As in Fig. 2, but at ten days after convective initiation.. Preferred ENSO Phase within Each Composite. Fig. 1: Histogram of ONI (°C) for (a) real MJOs and (b) failed MJOs. The sample size, mean, and standard deviation of each subset are provided in the top left corner of each histogram.. 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 . Brian Guyer & Deirdre Kann, National Weather Service, Albuquerque, NM. Project Summary. OBJECTIVE: . Test the growing suite of convective initiation products to determine their potential to improve forecasts and detection of hazardous convective events during the North American monsoon season.. . Insurance Trends and Challenges in an Era of Climate Volatility. National Tornado Summit. Oklahoma City, OK. February 11, 2014. Robert P. Hartwig, Ph.D., CPCU, President & Economist. Insurance Information Institute  110 William Street  New York, NY 10038. 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. 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. Courtney Schumacher for Brian’s 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). Ref Vel. stratiform. Conv(all) rad_ref. Cloud analysis followed by 3dvar. Conv(uv spd) rw. Only 3dvar analysis. Applied DFI to Qv only, other mosit variable like Qs, Qc, Qr, Qg, Qi are remain unchanged and. Physics 5403: Computational Physics. Physics. 5403: . Computational. . Physics. - . Chapter. 6: . Molecular. Dynamics. 1. 6.0 Overview. What is molecular dynamics (MD)?. Numerical method for studying many-particle systems such as molecules, clusters, and even macroscopic systems such as gases, liquids and solids . 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. 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..