HOLLY, COLORADO TORNADO 28 MARCH 2007 Bill Eckrich DayWeather, Inc. Cheyenne, Wyoming.

Slides:



Advertisements
Similar presentations
Daniel Nietfeld – NOAA/NWS/WFO Omaha NE Kansas City IWT Workshop: Using the WAS*IS Approach January 22, 2009.
Advertisements

Summer 2009 Western Fire Season Outlook Overview Significant fire potential is expected to be above normal across much of California, Florida, central.
February 19, 2004 Texas Dryline/Dust Storm Event.
Oklahoma’s Facts and Climate
X 3904 Woodcutter Drive SE Woodcutter Drive I-40 Westminster Road Path of Tornado.
The Lone Grove, OK, Tornado 10/02/2009 Robert Warren.
Tornado ! May 28, 1996.
WINTER WEATHER WRAP UP Mark Nelsen. WINTER FUN BEGINNING AND END, BUT “VANILLA” IN THE MIDDLE!
SPC Input – EMC GFS Satellite Data Denial Experiment April 2011 Tornado Outbreak Examination of Day 7 and Day 4 Guidance for SPC Severe Weather Outlooks.
A Comparison of Tornado Statistics from Tornado Alley and Dixie Alley
Analysis of Rare Northeast Flow Events By Joshua Beilman and Stephanie Acito.
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,
Super Tuesday Tornado Outbreak Presented by: Catherine Smith, Colleen Smith, Trevor Smith, Andrew Smith.
The Massachusetts Tornado Outbreak of June 1, 2011 Joe DelliCarpini Science and Operations Officer NOAA/NWS Taunton, MA.
October 20, 2014 Objective: I will be able to explain how, where, and why tornadoes form. Entry Task: DO NOT UNPACK – be ready for a new seating chart.
SPC Convective Outlook Changes Changes in Category Names/Definitions Bill Sammler Warning Coordination Meteorologist National Weather Service, Wakefield.
A Convective Wind Event over Southeastern Alberta on 15 July 2008 Stephen Knott and Chris Wielki Prairie and Arctic Storm Prediction Centre - Edmonton.
Article By: Charles Doswell III Donald V Baker Charles A Liles Presentation By: Jason Tiffany Recognition of Negative Mesoscale Factors for Severe-Weather.
An Overview of Environmental Conditions and Forecast Implications of the 3 May 1999 Tornado Outbreak Richard L. Thompson and Roger Edwards Presentation.
Anthony A. Rockwood Robert A. Maddox.  An unusually intense MCS produced large hail and wind damage in northeast Kansas and northern Missouri during.
THE DISTINCTION BETWEEN LARGE- SCALE AND MESOSCALE CONTRIBUTION TO SEVERE CONVECTION: A CASE STUDY EXAMPLE Paper by Charles A. Doswell III Powerpoint by.
Tornadoes. A violently rotating column of air, in contact with the ground, either pendant from a cumuliform cloud or underneath a cumuliform cloud, and.
Convective Initiation and Flow Regimes of Severe Storms Across the Central High Plains Scott F. Blair National Weather Service Goodland, Kansas.
Tornadic thunderstorm Dodge City, Kansas May 7, 2002  Large cumulonimbus anvil stretches from Missouri into eastern Kansas  Cumulonimbus anvil seen in.
2005 Tropical Weather Impacts to the Memphis CWA Jonathan L. Howell – Jason F. Beaman National Weather Service - Memphis, TN.
Severe Squall Line over Quebec August 18th 2008 Robert Michaud QSPC – Montreal October 29th 2008.
Synoptic, Thermodynamic, Shear Setting May 7, 2002 Tornadic Thunderstorm in Southwestern Kansas Michele Blazek May 15, 2005.
The 4 August 2004 Central Pennsylvania Severe Weather Event – Environmental and Topographical Influences on Storm Structure Evolution Joe Villani NOAA/NWS,
Chapter 10 – Midlatitude Cyclones. The Origin of the Theory of Midlatitude Cyclones The polar front theory (Norwegian cyclone model) – description of.
Use of TAMDAR Data in a Convective Weather Event Saturday, May 21, 2005.
May 31, 1985 Moshannon Forest Tornado By Henry Margusity Sr. Meteorologist AccuWeather.com.
Christopher S. Foltz Jeremy Martin Brad Mickelson NWS WFO Goodland, KS 13 th High Plains Conference August 2009.
George D. Phillips NOAA/NWS Weather Forecast Office, Topeka, Kansas.
An Evaluation of Mortality Rates Within the Path of Well-Warned Significant Tornadoes National Weather Service WFO Detroit, Michigan Joseph V Clark
Straight Line Winds are responsible for most thunderstorm wind damage winds can exceed 100 mph one type of straight line wind is called the downburst;
Mike Evans NWS / WFO BGM. CSTAR V – Severe convection in scenarios with low-predictive skill SUNY Albany researchers are examining SPC forecasts and associated.
National Weather Service Weather Forecast Office – Taunton, MA (BOX)
SYNOPTIC METEOROLOGY LABORATORY The Dallas and Fort Worth Storms of May 5, 1995 Storms of May 5, 1995 BY: Brent Crisp, Phil Grigsby, Thomas Jones, Devon.
1.Tornadoes are the most destructive of all weather- related events. 2. On average, a tornado's path is 2 miles long and 100 yards wide but can be as.
Composite Analysis of Environmental Conditions Favorable for Significant Tornadoes across Eastern Kansas Joshua M. Boustead, and Barbara E. Mayes NOAA/NWS.
TORNADOES!! Although tornadoes occur in many parts of the world, these destructive forces of nature are found most frequently in the United States east.
Tornadoes: What and why they occur Kevin Scott & Kevin Fitzgerald.
Trip planned Nov Duration  May 16 – May 24, 2013 Participants  Ohio State students & alum  Friends of the National Weather Service/Storm Prediction.
Dr. Jeff Basara’s Guide to Forecasting Severe Weather: Things to look for at the synoptic scale: Are there any regions of forced rising motion? What are.
The Dryline The dryline can be defined as the near surface convergence zone between moist air flowing off the Gulf of Mexico and dry air flowing off of.
Analysis of the 2 April 2006 Quasi-Linear Convective System (QLCS) over the Mid- Mississippi Valley Region: Storm Structure and Evolution from WSR-88D.
The 1925 Tri-State Tornado What If It Happened Today? Pat Spoden NOAA/NWS WFO Paducah, Kentucky John Hart NOAA/NWS Storm Prediction Center Norman, Oklahoma.
1 April 27-28, 2011 Southeast Tornado Outbreak April 27-28, 2011 ~190 tornadoes, ~311 fatalities Deadliest outbreak since March 21, 1932 Outlook issued.
WFO Huntsville, Alabama A Review of the North Alabama Violent Tornado Outbreak February 6, 2008 Brian Carcione & David Nadler NWS Huntsville, Alabama.
Forecasting Technique: Pattern Recognition Associating a “weather pattern” to a “weather event” Significant weather events have patterns –surface features.
Cool Season Tornadoes in the Southeast U.S. Steven Nelson Stephen Konarik WFO Peachtree City 11 November December January November.
A Review of the March 28, 2007 Tornado Event Teresa Keck NWS North Platte, Nebraska Courtesy of Mike Hollingshead.
2. Basic Characteristics and Forecast The 500-hPa pattern for this event featured a deep low centered over Idaho. A composite analysis of past tornado.
A Rare Severe Weather and Tornado Event in Central New York and Northeast Pennsylvania: July 8, 2014 Presented by Mike Evans 1.
*Special Webinar* Severe Storms Likely This Afternoon through Early Wednesday Tuesday February 23, 2016 Please MUTE Your Lines! *6 to Mute #6 to Unmute.
Tornadoes in the United States By: Katie Harris. Tornadoes are one of nature's most violent storms. In an average year, about 1,000 tornadoes are reported.
The April 9 th Tornado Outbreak Across the Four-State Region By Nick Fillo & Ismari Ramos WFO Shreveport, LA 4 th Regional Severe Storms/Radar and Hydrology.
Twenty-Three Foot Waves on Lake Michigan! Examining Storm Events on the Lake Mike Bardou and Kevin Birk Courtesy Mike Bardou.
For: East Tennessee, Southwest Virginia and far Southwest North Carolina When: Thursday Evening and Night Andrew Pritchett Valid: Thursday, March 31, 2016;
National Weather Service Weather Forecast Office Mobile - Pensacola Special Briefing Tropical Storm Lee Special Briefing Tropical Storm Lee 1030 AM CDT.
TORNADO.
National Weather Service Weather Forecast Office Mobile - Pensacola
February 24, 2016 Tornado Outbreak
ATM 401/501 Status of Forecasting: Spring 2013
CAE Tornado Cases Hunter Coleman Anthony Petrolito Michael Cammarata
An Investigation of the 26 July 2006 Downburst near Spearville, Kansas
A summary of Charles A. Doswell III’s:
Kansas 9/14/04 Tornado Distributed by the Disaster Team
THE TREND CONTINUES: MORE TORNADOES IN 2011 THAN IN 2010
Presentation transcript:

HOLLY, COLORADO TORNADO 28 MARCH 2007 Bill Eckrich DayWeather, Inc. Cheyenne, Wyoming

Overview of Holly, Colorado  Located in southeastern Colorado on U.S. Highway 50 in far eastern Prowers County, 28 miles east of Lamar and approximately 5 miles from the Kansas state line  Population 1,048 (2000 U.S. Census)

Holly Tornado Statistics  First touched down at 1957 MDT one mile south of Holly  WFO PUB Tornado Warning issued at 2000 MDT  Rated as high-end EF3  Moved just east of north across the entire town causing EF1 to low-end EF3 damage  2 fatalities, one within a day and another nearly a month later, with 10 injuries  Path length 28 miles over a minute period  Damage width in Holly was 1000 feet wide

Holly Tornado Statistics  48 structures destroyed  100+ structures damaged  Event occurred outside of both the SPC slight and moderate risk areas (12Z, 13Z, 1630Z, 20Z, 01Z) as well as the later-issued Tornado Watch #83  Colorado convection evolved from a retreating dryline possibly caused by stronger-than-forecast ageostrophic forcing from northward-propagating shortwave

SPC DAY1 OUTLOOK (20Z)

TORNADO WATCH #83 HOLLY

SYNOPTIC AND MESOSCALE ENVIRONMENT INCLUDING RADAR AND SATELLITE DATA

00Z 29 March 300mb NOSE OF JET STREAK

00Z 29 March 500mb

00Z 29 March 700mb

00Z 29 March 850mb THERMAL RIDGE

2116Z 28 March

2316Z 28 March

0200Z 29 March

IR SATELLITE 0100Z 29 MARCH

VISIBLE SATELLITE 0130Z 29 MARCH

0153Z 29 MARCH

0157Z 29 MARCH

0202Z 29 MARCH

HOLLY Prowers County Kiowa County Kansas

EF3 Damage in Holly WFO Pueblo

EF3 Damage in Holly WFO Pueblo

High-end EF3 Damage 12N of Holly WFO Pueblo

High-end EF3 Damage 12N of Holly WFO Pueblo

Courtesy Ty Harmon - KLMR

CONCLUSIONS  Large and deep storm system over the central Rockies  Large-scale ascent across eastern Colorado, southwestern Nebraska, western Kansas and the Oklahoma/Texas panhandles  Surface winds ahead of the dryline backed with time as the shortwave/jet streak approached  Dryline retreated  SRH increased with backing winds relative to storm motion

CONCLUSIONS  First tornado deaths in Colorado since June 27, 1960  Only the second killer tornado in Colorado since 1950  Earliest strong tornado in Colorado history Previous: 3/29/1910 in Sedgwick County  Earliest killer tornado in Colorado history Previous: 4/30/1942 in Bent/Kiowa counties

CONCLUSIONS  Prowers County has had only one prior significant tornado  June 24, 1968  One injury  Occurred within one mile of Holly