PPT-Severe convective storm modeling

Kay Cleary Director Regulatory Practice Meghan Purdy Associate Manager Model Solutions A recent survey What peril concerns you on a daytoday basis Has your company made changes to your severe weather ratemaking methodology in the last 3 years. Crystal K Williams. Department of Geography-Geology. Illinois State University. Outline. Introduction/Background. Mesoscale Convective Systems. Squall Lines. Precipitation. Conclusions. Introduction. 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. . 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. Tom Ravens and Jon Allen, Univ. of Alaska Anchorage. 10 km. 10 km. Kashunuk R.. Research Goal: determine the likely change in YK Delta ecology due to storm surges – enhanced by sea level rise. Tasks:. 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. Jonathan . Conder. WANE TV Chief Meteorologist. NWS-Media Relationship. My goal as a broadcast meteorologist:. Provide the most accurate and precise forecast and the most immediate and detailed severe weather coverage. 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. NCEP . Production Suite Review. December . 7, 2015. Steven . Weiss, Russell Schneider, Israel . Jirak. , Chris . Melick. , Andy Dean, and Patrick Marsh. Storm Prediction Center, Norman, OK. National Weather Center. -1. CIN extending upwards to 800 . hPa. and < 500 J kg. -1 . CAPE. . . There was 41.8 mm of . precipitable. water. . By 1400 UTC, CIN in RAP analysis decreased to 93 J kg. -1 . and CAPE increased to 1743 J kg. 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. From . www.spc.noaa.gov/faq/#4.2. , SPC defines a thunderstorm as severe if it has one of more of the following:. a. Hail at least 1 inch in diameter (quarter size). b. Wind gusts to 58 mph or greater (50 knots). Dr. Steve Koch. NOAA/OAR/National Severe Storms Laboratory. Dr. Bruce Baker. NOAA/OAR/Air Resources Laboratory. July 27, 2016. Needs vs. Requirements. Spatial resolution. (km). Vertical resolution. (m). 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..