PPT-Synoptic Environments Associated with the Training of Convective Cells

Synoptic Environments Associated with the Training of Convective Cells Aylward and Dyer 2010 The main focus is investigating the dynamics resulting in synoptically forced training convective rainfall. p.connolly@manchester.ac.uk Introduction: Convective invigoration describes a pathway by which aerosols modulate cloud evolution, precipitation and radiation (Rosenfeld et al. 2008). This idea sugges Stephen Rodriguez, Jr.. National Weather Service Chicago, IL. Introduction. Brief background.. Purpose of Study.. Synoptic background and forcing mechanisms.. Synoptic/. Mesoscale. features: Moisture, Forcing, Instability.. 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.. . E. CHAM5-HAM. B. Croft. 1. , J.R. . . Pierce. 1. , R.V. Martin. 1,2. , C. Hoose. 3. , and U. Lohmann. 4. 1. Dalhouse University, Canada. 2. Harvard-Smithsonian Centre for Astrophysics, USA. 3. Karlsruhe Institute of Technology, Germany. http://www.ucar.edu/communications/factsheets/Tornadoes.html. Packet#1. What is meant by “Mesoscale Meteorology”?. ATMS 316- Mesoscale Meteorology. http://www.ucar.edu/communications/factsheets/Tornadoes.html. 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. Doswell C.A. III, 2001: Severe Convective Storms – An Overview. Severe Convective Storms, Meteor. Monogr., 28, no. 50, Amer. Meteor. Soc., 13-26. General Outline of this Review. Severe Convection Definitions & Distinctions. 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. Course Overview & Logistics. Wed – 20 Aug 2014. Introductions…. Office: NSSTC 3088. Email: . ryan.wade@uah.edu. Phone: 961-7847 (office phone). Office Hours. :. MWF: 8:00am – 9:00am, 10:15am – 11:00am. 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. Presenter:. Kelli K. Olsen, MS, CTR. Cancer Registry Administrator at City of Hope. Co-Authors: . Rebecca A. Ottesen, MS, Leanne Goldstein, . DrPH. , Janet Nikowitz, CTR, Julie A. Kilburn, and Joyce . Most Conducive to North American . Polar/Subtropical Jet . Superpositions. Andrew C. Winters. 2 August 2018. This work is funded by an NSF-PRF (AGS-1624316). Modified from . Defant. and . Taba. (1957). Kerry Emanuel. Massachusetts Institute of Technology. Several Possibly Inter-related Enigmas of the Tropical Atmosphere. Why does moist convection often cluster?. What determines the number of tropical cyclones on the planet?.