PPT-Leveraging Total Lightning and Convective Initiation Data for Impact-Based Decision Support

Brian Carcione WFO Huntsville AL Background Total Lightning WFO HUN has a long history 11 yrs with SPoRT and Total Lightning from North Alabama Lightning Mapping Array Convective Initiation from . . 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. Goodman. , Richard Blakeslee, William Koshak, and Douglas Mach. with contributions from the GOES-R GLM AWG and Science Team. 1. GOES-R Program Senior Scientist, NOAA/NESDIS GPO. 2. UA Huntsville. http://www.goes-r.gov. RITT Presentation. Tom Filiaggi (NWS – MDL). 12/18/13. Reduction of FAR?. Agenda. Team Members. Total Lightning. Lightning Mapping Arrays (LMAs). Previous Research Summary. Current Project. Analysis & Results. RITT Presentation. Tom Filiaggi (NWS – MDL). 11/28/12. Evaluation of “. 2. σ. ” as Predictor for Severe Weather. Agenda. Total Lightning. Lightning Mapping Arrays (LMAs). Previous Research Summary. Tim Dennis – Solution Consultant, QAD. 2. The following is intended to outline QAD’s general product direction. It is intended for information purposes only, and may not be incorporated into any contract. It is not a commitment to deliver any material, code, functional capabilities, and should not be relied upon in making purchasing decisions. The development, release, and timing of any features or functional capabilities described for QAD’s products remains at the sole discretion of QAD.. Chattanooga, Tennessee (Hamilton County) For Public Safety and Decision Making. What is the utility of . using Lightning Mapping Array (LMA) . data for public safety and decision making for Emergency Management?. Christopher J. Schultz. 1. , Lawrence . D. . Carey. 2. , Walter A. Petersen. 3. , Daniel Cecil. 2. , Monte Bateman. 4. , Steven Goodman. 5. , Geoffrey Stano. 6. , Valliappa Lakshmanan. 7. 1 - Department of Atmospheric Science, . 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. Mesoscale. Convective Systems. Trent Davis. 25 April, 2017. Background. Well known that most flashes occur within leading convective line, fewer in trailing stratiform region (SR). Most of CGs (mainly -) occur in convective line (CL). Lightning Jump Evaluation RITT Presentation Tom Filiaggi (NWS – MDL) 12/18/13 Reduction of FAR? Agenda Team Members Total Lightning Lightning Mapping Arrays (LMAs) Previous Research Summary Current Project Purpose of initiation phase. Comparing project options. Total cost of ownership. The project charter. The Initiation Phase. Business problem or opportunity defined. Solution is defined. Project is formed. 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?. Kengo. . Matsubayashi. Japan Meteorological Agency. The Met Office. Outline. Motivation. Observation and evaluation method. Evaluation result. Summary. In many convection schemes, water substances are empirically modelled.. 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..