PPT-Quasi-stationary Convective Storms in the UK: A Case Study

Robert Warren Supervised by Bob Plant Humphrey Lean amp Dan Kirshbaum Background Quasistationary convective storms QSCSs Repeated triggering and training of cells over a localised area for an extended period of time. Robert Warren. 2. Contents. My background. Introduction & Motivation. Project aims and methodologies. Work so far. Background reading. Boscastle. Flood. Case studies. 21/07/2010. Work going forward. 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.. MINERvA. Kevin McFarland. University of Rochester. NuINT11, Dehradun. 8 March 2011. ν. Goddess′. μ. To India . via. Indiana. Thank you to the organizers . for their efforts to allow me to attend . Tamara . McDunn. 1. . Advisor. : David . Kass. 1. 1. Jet . Propulsion Laboratory, California Institute of . Technology. JPL Postdoc Seminar, June 27, 2013. CL#13-. 1687. (c) 2013 California Institute of Technology. Government sponsorship acknowledged.. 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. &. 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.. 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. How Is Snow Formed?. Snow is commonly formed when water vapor undergoes deposition, which is when water vapor changes directly to ice without first becoming a liquid.. High in the atmosphere at a temperature of less than 32 degrees Fahrenheit and then falls to the ground.. Show direct cause & effect. Study relationships among variables for existing groups. Explain outcomes after the fact. Type of Design. True Experiment. Quasi-Experiment. Cross-Sectional. Longitudinal. Betsy Berry and Jay Mace. University of . Utah. American Geophysical Union 2011 . Fall Meeting. More CCN→. more small droplets→ . less collision→ delayed raindrop formation . Smaller sizes are lofted higher where they freeze→ latent heat release leads to increased buoyancy and a stronger updraft. by . Addison . Beckemeyer. . &. . Thao. Tran . Zwitterionic Stationary Phase in HPLC. Outline. Introduction . Theory . Advantages and Disadvantages. Some Applications. Conclusions. References . Getting started. You’ll need a notepad on which to make notes as you go along, or you could make notes, paste images, etc. on your device.. You can view these slides:. as a slide-show for any animations and to follow links. Based on the ITER-like and Snowflake divertor configuration of CFETR (Phase I, R = 5.7 m), SOLPS simulation is performed to understand the performance of radiative quasi-snowflake . divertor . with argon seeding.. on a curve. Find the coordinates of. a stationary point on a curve. Identify whether a stationary point is a maximum, minimum or inflexion point. Stationary Points. A stationary point is where the gradient is 0, i.e. .