Using The Short Fuse Composite to Forecast Severe Convection: Part I– Ancient History; The AFOS Era By Jim Johnson & Mike Umscheid NWS Dodge City, KS.

Slides:



Advertisements
Similar presentations
Last Lab: (Hail formation) Anthony R. Lupo Atms 4310 / 7310 Lab 13.
Advertisements

Forecasting convective outbreaks using thermodynamic diagrams. Anthony R. Lupo Atms 4310 / 7310 Lab 10.
What idiot is wasting our storm-chasing time talking about a winter storm? The New Year’s Day Storm in Central Minnesota Robert A. Weisman, Saint Cloud.
A Forecasting Success A negatively tilting mid level trough approaching North Carolina, combined with strong instability and increasing deep layer shear,
Correlations between observed snowfall and NAM “banded snowfall” forecast parameters Mike Evans and Mike Jurewicz WFO BGM.
Warm Season Frontogenesis Forcing Applications and Implications for Convective Initiation (or Failure) Dan Miller Science and Operations Officer NWS/WFO.
National Weather Service Protecting Lives and Property Precipitation Potential Placement ER Flash Flood Workshop Jeff Myers/Jim Noel NOAA/NWS/OHRFC
Aspects of 6 June 2007: A Null “Moderate Risk” of Severe Weather Jonathan Kurtz Department of Geosciences University of Nebraska at Lincoln NOAA/NWS Omaha/Valley,
Visually Enhanced Composite Charts for Severe Weather Forecasting and Real-time Diagnosis Josh Korotky NWS Pittsburgh PA NROW Annual Meeting 2002.
My grandparents’ farm or so The farm NW of Sac City near Nemaha.
Mike Evans / NWS Binghamton, NY. Outline Large-scale pattern / meso-analysis Radar data High resolution model output Summary.
An Overview of Environmental Conditions and Forecast Implications of the 3 May 1999 Tornado Outbreak Richard L. Thompson and Roger Edwards Presentation.
Kari Murray.  This article is extending on a 10-year climatological study done by Rose et al.  Rose et al. found that tornadoes most commonly occur.
The supercell storm Anthony R. Lupo Atms 4310 / 7310 Lab 12.
Case (Chase) Study: 04 May 2007 Supercells, Supercells, and more Supercells.
Extratropical Synoptic-Scale Processes and Severe Convection Part 1 Elizabeth Polito Pg ( ) Part 2 Terrance Seddon pg ( )
RECENT PROGRESS IN CONVECTIVE PHENOMENA MONITORING AND FORECASTING AT THE INM F. Martín, F. Elizaga, I. San Ambrosio and J. M. Fernández Servicio de Técnicas.
A Storm-Scale Analysis of the 16 June 2008 Significant Severe Weather Event across New York and Western New England Thomas A. Wasula NOAA/NWS at Albany.
Influence of tropopause-level disturbances on convection Geraint Vaughan.
Chapter 13 – Weather Analysis and Forecasting. The National Weather Service The National Weather Service (NWS) is responsible for forecasts several times.
Roll or Arcus Cloud Supercell Thunderstorms.
Corfidi, et al – convection where air parcels originate from a moist absolutely unstable layer above the PBL. Can produce severe hail, damaging.
Review for Final Exam. Final Exam Tuesday December 17 th, 5pm-7:30pm Room CC301 (this room) 25% of final grade Combination of quick general questions.
Simulating Supercell Thunderstorms in a Horizontally-Heterogeneous Convective Boundary Layer Christopher Nowotarski, Paul Markowski, Yvette Richardson.
Lecture 2a Severe Thunderstorm Primer Synoptic Laboratory II – Mesoscale Professor Tripoli.
Shear Lines, Fronts and Areas of Confluence/Diffluence Mike Davison HPC International Desks.
Using The Short Fuse Composite to Forecast Severe Convection: Part II – “The Next Generation,” Updating the Technique By Jim Johnson & Mike Umscheid NWS.
NON-MESOCYLONE TORNADOGENESIS IN THE 26 OCTOBER 2006 CLOSED MID LEVEL LOW SEVERE CONVECTIVE EVENT Aaron Johnson NWS Dodge City KS.
Henry Fuelberg Pete Saunders Pendleton, Oregon Research Region Map Types and Lightning Frequencies.
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 Image: MODIS Land Group, NASA GSFC March 2000 Nearcasting Severe Convection.
Soundings and Adiabatic Diagrams for Severe Weather Prediction and Analysis Continued.
WV images to diagnose the context favourable for deep convection Patrick Santurette Forecast Laboratory METEO-FRANCE Christo Georgiev National Institute.
Forecast Parameters. CAPE Convective Available Potential Energy – obviously, positive buoyancy is helpful for producing convection –100 mb mixed layer.
Isentropic Analysis of January Snowstorm Across Eastern Virginia and Lower Maryland Tim Gingrich and Brian Hurley NOAA/NWS Wakefield VA Isentropic.
Soundings and Adiabatic Diagrams for Severe Weather Prediction and Analysis.
Summer Tornadoes – NWA 2015 Statistical Severe Convective Risk Assessment Model (SSCRAM) (Hart & Cohen, 2015) SPC Mesoanalysis Data Every hour from
Extending Geostationary Satellite Retrievals from Observations into Forecasts Using GOES Sounder Products to Improve Regional Hazardous Weather Forecasts.
Statistical Severe Convective Risk Assessment Model (SSCRAM) SPC Mesoanalysis Data every hour from (Bothwell et al. 2002) + CG NLDN Lightning.
Travis Smith, Jidong Gao, Kristin Calhoun, Darrel Kingfield, Chenghao Fu, David Stensrud, Greg Stumpf & a cast of dozens NSSL / CIMMS Warn-on-Forecast.
Applied Meteorology Unit 1 High Resolution Analysis Products to Support Severe Weather and Cloud-to-Ground Lightning Threat Assessments over Florida 31.
Examining the Role of Mesoscale Features in the Structure and Evolution of Precipitation Regions in Northeast Winter Storms Matthew D. Greenstein, Lance.
Center for Satellite Applications and Research (STAR) Review 09 – 11 March 2010 Image: MODIS Land Group, NASA GSFC March 2000 Nearcasting Severe Convection.
Severe Thunderstorm Summary METR 361. The Pre-storm Environment On the Surface map, look for: On the Surface map, look for: 1.Warm air, T > 50 F 2.High.
Soundings and Adiabatic Diagrams for Severe Weather Prediction and Analysis Continued.
Cirrus anvil cumulonimbus T (skewed) LCL (Lifting Condensation Level) LFC (Level of Free Convection) EL (Equilibrium level) p overshooting CAPE Sounding.
Class #26: Friday October 30 Thunderstorms 1Class #26: Friday, October 30, 2009.
The apparent movement of the sun while being viewed on Earth is caused by the rotation of the Earth The Earth spins much like a top It makes a complete.
Defining a Threat Area and Miller Techniques
Thermodynamics We Can See!
Soundings and Adiabatic Diagrams for Severe Weather Prediction and Analysis Ooohhhh!!!!!!!!!!! Aaaahhhhhhhh!!!!!! Look at the pretty picture!
anelastic: Boussinesque: Homework 1.1 …eliminates sound waves
Michael K. Tippett1,2, Adam H. Sobel3,4 and Suzana J. Camargo4
Thunderstorms Features Cumulonimbus clouds Heavy rainfall Lightning
Comparison of Observed Conditions with Stability Indices
Lightning Potential Index (J/Kg) (Yair et al.2010,JGR)
Lightning Potential Index (J/Kg) (Yair et al.2010,JGR)
Lightning Potential Index (J/Kg) (Yair et al.2010,JGR)
Lightning Potential Index (J/Kg) (Yair et al.2010,JGR)
Lightning Potential Index (J/Kg) (Yair et al.2010,JGR)
Lightning Potential Index (J/Kg) (Yair et al.2010,JGR)
Lightning Potential Index (J/Kg) (Yair et al.2010,JGR)
Lightning Potential Index (J/Kg) (Yair et al.2010,JGR)
Lightning Potential Index (J/Kg) (Yair et al.2010,JGR)
Lightning Potential Index (J/Kg) (Yair et al.2010,JGR)
Lightning Potential Index (J/Kg) (Yair et al.2010,JGR)
Lightning Potential Index (J/Kg) (Yair et al.2010,JGR)
Lightning Potential Index (J/Kg) (Yair et al.2010,JGR)
Lightning Potential Index (J/Kg) (Yair et al.2010,JGR)
Lightning Potential Index (J/Kg) (Yair et al.2010,JGR)
Lightning Potential Index (J/Kg) (Yair et al.2010,JGR)
Presentation transcript:

Using The Short Fuse Composite to Forecast Severe Convection: Part I– Ancient History; The AFOS Era By Jim Johnson & Mike Umscheid NWS Dodge City, KS

Using The Short Fuse Composite to Forecast Severe Convection:  The Dark Ages  Phil Bothwell's ADAP (NWS SR-114) piped in from AFOS node in  Watched hourly ADAP charts for May 7, 1986 Canadian, TX F-3.  A few base charts selected by spring season of STA, SMC, SSL and SSC.  Charts watched for 18 TX, KS and CO Tornadoes Epiphany!! Nov. 15, 1988 TOP  Empirical values noted by parameter - composite the charts and define a threat area.

Using The Short Fuse Composite to Forecast Severe Convection: Parameters: Flux Divergence of Surface Mixing Ratio Potential Temperature Advection Surface to 500 hPa Lifted Index Convective Cap Streamlines of Surface wind direction Thru 1996 total of 63 cases – 81% success in first hour from composite time – 62% in second hour…

Using The Short Fuse Composite to Forecast Severe Convection: The Short Fuse Threat Area  Down-wind of the positive Theta advection axis. (ex. - Burgess, et al. BAMS, 1994)  Within the 1.5g/kg/hr SMFC isopleth. (Waldstreicher, NWA Dig.,14, 1989)  On axis of maximum instability  Convective “cap” 2 degrees Celsius or less. Tornado Symposium III 1990 – AGU Monograph 79 Went online in 1996 – heavy use by chasers

Using The Short Fuse Composite to Forecast Severe Convection:

*TORN 1 S Amorita OK 25/0045Z *TORN 3 ENE Amorita OK 25/0050Z *TORN 8 E Amorita OK 25/0055z-0105Z *TORN 6 W Medford OK 25/0146Z-0153Z Total 15 Tornadoes – Cyclic Supercell?

Using The Short Fuse Composite to Forecast Severe Convection:  Change to AWIPS and associated problems – MSAS and LAPS aren’t same as ADAP!  AWIPS can’t do O.A. of raw data!!  When AFOS was unplugged, so was the composite!  Had to find a way to apply the technique to AWIPS product sets - recalling that the previously arrived at empirical values were no longer valid……..