Storm Spotter Through Technology & Education Enhancements
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The Birth and Early Years of the Storm Prediction Center
AUGUST 1999 CORFIDI 507 The Birth and Early Years of the Storm Prediction Center STEPHEN F. C ORFIDI NOAA/NWS/NCEP/Storm Prediction Center, Norman, Oklahoma (Manuscript received 12 August 1998, in ®nal form 15 January 1999) ABSTRACT An overview of the birth and development of the National Weather Service's Storm Prediction Center, formerly known as the National Severe Storms Forecast Center, is presented. While the center's immediate history dates to the middle of the twentieth century, the nation's ®rst centralized severe weather forecast effort actually appeared much earlier with the pioneering work of Army Signal Corps of®cer J. P. Finley in the 1870s. Little progress was made in the understanding or forecasting of severe convective weather after Finley until the nascent aviation industry fostered an interest in meteorology in the 1920s. Despite the increased attention, forecasts for tornadoes remained a rarity until Air Force forecasters E. J. Fawbush and R. C. Miller gained notoriety by correctly forecasting the second tornado to strike Tinker Air Force Base in one week on 25 March 1948. The success of this and later Fawbush and Miller efforts led the Weather Bureau (predecessor to the National Weather Service) to establish its own severe weather unit on a temporary basis in the Weather Bureau± Army±Navy (WBAN) Analysis Center Washington, D.C., in March 1952. The WBAN severe weather unit became a permanent, ®ve-man operation under the direction of K. M. Barnett on 21 May 1952. The group was responsible for the issuance of ``bulletins'' (watches) for tornadoes, high winds, and/or damaging hail; outlooks for severe convective weather were inaugurated in January 1953. -
Weather Spotter Training 2019
Weather Spotter Training 2019 NOAA/National Weather Service Weather Forecast Office Salt Lake City, UT Goals of the Training You will learn: • Definitions of important weather terminology and extreme weather criteria • How to correctly identify significant weather features and events • What information the spotter is to report and how to report it Near Grantsville, UT - September 4, 2007 • Ways to receive weather information before and during extreme weather events • Spotter Safety About the National Weather Service (NWS) Provides weather, hydrologic, and climate forecasts and warnings for the protection of life and property and the enhancement of the national economy Salt Lake City Weather Forecast Office (WFO) prepares and issues forecasts and warnings for 26 counties in Utah and extreme southwest Wyoming 24/7 Operation Past Weather Events Severe Thunderstorms/Tornadoes Floods/Flash Floods Debris Flows Winter Storms Wildland Fires Lightning Windstorms Severe Thunderstorms/Tornadoes Photo courtesy KSL West Jordan Microburst August 5, 2013 37 large transmission poles and 4 smaller distribution poles 3,000 customers lost power State Route 111 closed $300,000 dollars damage Severe Thunderstorms/Tornadoes Riverdale/Washington Terrace/South Ogden Tornado September 22, 2016 Enhanced Fujita (EF) Scale - EF1 Track length – nearly 3 miles Max width - approximately 50 yards 5 injuries Total damage - $2,000,000 Severe Thunderstorms/Tornadoes Panguitch Tornado September 22, 2016 Enhanced Fujita (EF) Scale – EF1 Track length - three-quarters of a -
The Educational Training of Storm Chasers and Storm Spotters in Relation to Geographical Dispersion Across the United States
Minnesota State University, Mankato Cornerstone: A Collection of Scholarly and Creative Works for Minnesota State University, Mankato Theses, Dissertations, and Other Capstone Projects 2013 The ducE ational Training of Storm Chasers and Storm Spotters in Relation to Geographical Dispersion Across the United States Paul R. Zunkel Minnesota State University - Mankato Follow this and additional works at: http://cornerstone.lib.mnsu.edu/etds Part of the Meteorology Commons, and the Physical and Environmental Geography Commons Recommended Citation Zunkel, Paul R., "The ducaE tional Training of Storm Chasers and Storm Spotters in Relation to Geographical Dispersion Across the United States" (2013). Theses, Dissertations, and Other Capstone Projects. Paper 140. This Thesis is brought to you for free and open access by Cornerstone: A Collection of Scholarly and Creative Works for Minnesota State University, Mankato. It has been accepted for inclusion in Theses, Dissertations, and Other Capstone Projects by an authorized administrator of Cornerstone: A Collection of Scholarly and Creative Works for Minnesota State University, Mankato. The Educational Training of Storm Chasers and Storm Spotters in Relation to Geographical Dispersion Across the United States By Paul Zunkel A Thesis Submitted in partial Fulfillment of the Requirements for Master of Science Degree in Geography Minnesota State University, Mankato Mankato, Minnesota May 2013 5 April, 2013 This thesis has been examined and approved. Examining Committee: Dr. Forrest Wilkerson, Chairperson Dr. Ginger Schmid Dr. Cynthia Miller ACKNOWLEDGEMENTS This research paper is dedicated to Mrs. Hope Hislop. Thank you for all the years of guidance, encouragement, and advice about following my dreams and pursuing my passions. No one could ask for a better grandmother. -
Advanced Weather Spotting for the Inland Northwest
Advanced Weather Spotting for the Inland Northwest Spring 2021 National Weather Service - Spokane Clyde, WA - Dave Brock May 2020 This is a Live Virtual Class ● Voice in Computer - no phone needed - headphones helpful ● All are in listen mode until the end Objectives ● Understand the roles & importance of the Weather Spotter ● Describe your community’s severe weather threats ● Provide accurate and timely reports of severe weather ● Properly define a severe thunderstorm and basic thunderstorm structure ● Identify cloud types and features of thunderstorms. ● Learn how to prepare and be safe during severe weather Concentration on Thunderstorms and Severe Weather Risk Awareness Now let’s look back to last year… June 24, 2020 - Severe Thunderstorm Event Ritzville Suncrest North of Tri Cities Pullman Colfax Pullman Palouse May 30, 2020 - Severe Thunderstorm Event Ritzville Suncrest Clyde - Dave Brock Blowing Dust - Ritzville Pullman Palouse May 2, 2020 - Thunderstorm & Dust Event Suncrest Ritzville North of Tri Cities Pullman Colfax Clyde - Dave Brock Blowing Dust - Ritzville Pullman Post Falls, ID Palouse To our current Weather Spotters…. THANK YOU! Eyes and Ears of the National Weather Service with a count of over 1200 across the Inland NW! National Weather Service (NWS) •Part of the Federal Government – Dept of Commerce •Responsible for all weather/water Watches & Warnings •126 offices across the country •Work with local agencies NWS Spokane •Observe & Forecast •“Behind the Scenes” •Decision Support •Preparedness & Education Issue Weather -
Storm Observation
Storm Observation The Basics of Severe Thunderstorms and Tornadoes By Ethan Schisler Introduction • About Me: • Storm Chasing since 2003 • Have chased from Montana to Florida • Observed over 100 tornadoes • Several strong hurricanes • Blizzards • Ice Storms Goal: Minimize the risks and maximize the positives Introduction • Storm Observation Can Be: • Exciting • Rewarding • Awe Inspiring • Fun • And Informative • Storm Observation Can Also Be…. • Dangerous • Time Consuming • And even costly….. Goal: Minimize the risks and maximize the positives • EF0 to EF5 • EF0 – 60-85 mph • EF1 – 86-110 mph • EF2 – 111-135 mph • EF3 – 136-165 mph • EF4 – 166-200 mph • EF5 – 200+ mph Enhanced Fujita Scale Why Storm Spotting? • Limitations in Doppler Radar • Warning Verification • To gain additional knowledge July 19 2018: Marshalltown, IA -Large EF-3 Tornado impacts town -Up to 43 minutes lead time -Only minor injuries and no deaths –Attributed to advanced warning, radar, and storm spotters! Storm Observation: Equipment • Cell phone/computer with radar application • Radarscope (Iphone, Mac, Windows); PYKL3 (Android); GR Level 3 (Windows) • Reliable vehicle to get from point A to point B • A partner to navigate • Stay distraction free while driving to the target area or storms • Video camera or still camera for documentation • Road maps and weather radio • Cell phone data can be sketchy in rural areas…have a backup plan • Marginal Risk • Slight Risk • Moderate Risk • High Risk Storm Prediction Center Outlooks Basics of Storm Development • Instability • -
Severe Deep Moist Convective Storms: Forecasting and Mitigation David L
Geography Compass 2/1 (2008): 30–66, 10.1111/j.1749-8198.2007.00069.x SevereBlackwOxford,GECOGeography17©J06910.Oct030???66???Origournal 49-819820071111/jober inal deepell ComT UK2007Art.he17 Publishing Com icles 49-8Autmoist pilatho pass 198io rconvective n .©2007 Lt 2007d .00069. Blackw stormsx ell Publishing Ltd Severe Deep Moist Convective Storms: Forecasting and Mitigation David L. Arnold* Department of Geography, Frostburg State University Abstract Small-scale (2–20 km) circulations, termed ‘severe deep moist convective storms’, account for a disproportionate share of the world’s insured weather-related losses. Spatial frequency maximums of severe convective events occur in South Africa, India, Mexico, the Caucasus, and Great Plains/Prairies region of North America, where the maximum tornado frequency occurs east of the Rocky Mountains. Interest in forecasting severe deep moist convective systems, especially those that produce tornadoes, dates to 1884 when tornado alerts were first provided in the central United States. Modern thunderstorm and tornado forecasting relies on technology and theory, but in the post-World War II era interest in forecasting has also been driven by public pressure. The forecasting process begins with a diagnostic analysis, in which the forecaster considers the potential of the atmos- pheric environment to produce severe convective storms (which requires knowl- edge of the evolving kinematic and thermodynamic fields, and the character of the land surface over which the storms will pass), and the likely character of the storms that may develop. Improvements in forecasting will likely depend on technological advancements, such as the development of phased-array radar sys- tems and finer resolution numerical weather prediction models. -
Tornado Basics
TORNADO BASICS NOAA/National Weather Service Tornado FAQ What is a tornado? According to the Glossary of Meteorology (AMS 2000), a tornado is "a violently rotating column of air, pendant from a cumuliform cloud or underneath a cumuliform cloud, and often (but not always) visible as a funnel cloud." Literally, in order for a vortex to be classified as a tornado, it must be in contact with the ground and the cloud base. Weather scientists haven't found it so simple in practice, however, to classify and define tornadoes. For example, the difference is unclear between an strong mesocyclone (parent thunderstorm circulation) on the ground, and a large, weak tornado. There is also disagreement as to whether separate touchdowns of the same funnel constitute separate tornadoes. It is well- known that a tornado may not have a visible funnel. Also, at what wind speed of the cloud-to-ground vortex does a tornado begin? How close must two or more different tornadic circulations become to qualify as a one multiple-vortex tornado, instead of separate tornadoes? There are no firm answers. BACK UP TO THE TOP How do tornadoes form? The classic answer -- "warm moist Gulf air meets cold Canadian air and dry air from the Rockies" -- is a gross oversimplification. Many thunderstorms form under those conditions (near warm fronts, cold fronts and drylines respectively), which never even come close to producing tornadoes. Even when the large-scale environment is extremely favorable for tornadic thunderstorms, as in an SPC "High Risk" outlook, not every thunderstorm spawns a tornado. The truth is that we don't fully understand. -
Cover Photo - Alan Moller I
Cover Photo - Alan Moller I. INTRODUCTION Objectives of this Handbook During the past several years, researchers have uncovered a tremendous amount of information regarding severe thunderstorm The Spotter’s Role structure and behavior. New theories regarding thunderstorm formation and tornado development have been presented. Storm- The National Weather Service (NWS) has a number of devices for intercept teams have correlated these theories with observed visual detecting severe thunderstorms. Included in these are radar, satel- features. Our current understanding of the thunderstorm is lite, and lightning detection networks. However, the most important markedly more complete than it was just ten years ago. tool for observing thunderstorms is the trained eye of the storm spotter. While radar is used quite often in severe storm warnings, With this handbook and the Advanced Spotter Training Slide Set conventional weather radar will only indicate areas and intensities which was released a few years ago, the time has come to pass this of precipitation. It does not give any indication of cloud formations new understanding on to you, the spotter. Only by providing fresh or wind fields associated with a storm. Doppler radar, which is training material can the NWS expect to maintain what has become being introduced across the country, will give some indication of air a very important group of observers. motions inside a storm. Doppler radar, though, will not give these indications down to ground level. It is impossible for any radar to detect every severe weather event in its coverage area, and radar Prerequisites for Using this Guide occasionally suggests severe weather when, in fact, none is present. -
Severe Weather Awareness
Severe Weather Awareness English 314 Proposal 2010 Authored by: Elizabeth Suess Samantha Santeiu Ryan Alliss Severe Weather Awareness English 314 Proposal Table of Contents SITUATION ............................................................................................................................ 2 WATCH : ............................................................................................................................ 2 WARNING : ........................................................................................................................ 3 TELEVISION ....................................................................................................................... 3 WEATHER RADIOS ............................................................................................................. 3 CIVIL DEFENSE SIRENS ...................................................................................................... 4 PLAN .................................................................................................................................... 4 BENEFITS .............................................................................................................................. 5 FLIERS .............................................................................................................................. 5 WEBSITE ........................................................................................................................... 5 SURVEYS .......................................................................................................................... -
Presentation
7.A.1 TROPICAL CYCLONE TORNADOES – A RESEARCH AND FORECASTING OVERVIEW. PART 1: CLIMATOLOGIES, DISTRIBUTION AND FORECAST CONCEPTS Roger Edwards Storm Prediction Center, Norman, OK 1. INTRODUCTION those aspects of the remainder of the preliminary article Tropical cyclone (TC) tornadoes represent a relatively that was not included in this conference preprint, for small subset of total tornado reports, but garner space considerations. specialized attention in applied research and operational forecasting because of their distinctive origin within the envelope of either a landfalling or remnant TC. As with 2. CLIMATOLOGIES and DISTRIBUTION PATTERNS midlatitude weather systems, the predominant vehicle for tornadogenesis in TCs appears to be the supercell, a. Individual TCs and classifications particularly with regard to significant1 events. From a framework of ingredients-based forecasting of severe TC tornado climatologies are strongly influenced by the local storms (e.g., Doswell 1987, Johns and Doswell prolificacy of reports with several exceptional events 1992), supercells in TCs share with their midlatitude (Table 1). The general increase in TC tornado reports, relatives the fundamental environmental elements of noted as long ago as Hill et al. (1966), and in the sufficient moisture, instability, lift and vertical wind occurrence of “outbreaks” of 20 or more per TC (Curtis shear. Many of the same processes – including those 2004) probably is a TC-specific reflection of the recent involving baroclinicity at various scales – appear to major increase in overall tornado reports, particularly contribute to tornado production in both tropical and those of the weakest (F0/EF0) damage category in the midlatitude supercells. TCs do diverge somewhat from database. -
Severe Weather Planning for Schools
Severe Weather Planning for Schools National Clearinghouse for Educational Facilities Barbara McNaught Watson, Christopher Strong, and Bill ball fields during little league and soccer games. Many Bunting, National Weather Service1 games are not called until the rain begins, and yet it is 2008 not the rain that is dangerous. Ball fields provide a lot of potential lightning targets such as poles, metal fences, and metal bleachers. The fields themselves are wide Understanding the Danger open areas where players are often the tallest objects around. Scenario 1. Lightning Strike Lightning is the most common thunderstorm threat. It’s a warm afternoon and the football team is on the field Nationally, lightning kills an average of over 70 people practicing. Some parents and a few other spectators sit annually and injures hundreds more. This number may in the bleachers watching the play. The sky to the west not seem high, yet when you look at the individual is darkening and a warm breeze has picked up. The cases, most could have been prevented. The basic rule rumble of thunder can be heard in the distance. Keeping of thumb is “If you can hear thunder, you are close a watchful eye to the sky, the coach figures he can get enough to the storm to be struck!” Thunderstorms through most of the practice before the rain comes. extend 5 to 10 miles into the atmosphere. Winds aloft There is a big game on Saturday and only one practice can blow the upper portion (anvil) of the storm many left. He can’t afford to let up now. -
2013 Conference Booklet
THE FOURTEENTH SOUTHERN NEW ENGLAND WEATHER CONFERENCE OCTOBER 26, 2013 Medical Information Technology, Inc. (MediTech) Canton, MA Sponsored by: Blue Hill Observatory Science Center National Weather Service - Taunton, MA UMass-Lowell Student Chapter of the American Meteorological Society Lyndon State College Chapter of the AMS/National Weather Association Foreword Welcome to the Fourteenth Southern New England Weather Conference! The purpose of the conference is to enhance professional development and communication among private and public sector meteorologists, teachers, emergency management officials, and weather enthusiasts. This year, we will be focusing a lot of talks about Superstorm Sandy from 2012. However, we will also cover a wide variety of subject areas, including the 1938 hurricane, blizzards, tornadoes, risk management, decision support services, and some good information for teaching weather in the classroom. Superstorm Sandy affected New Jersey, New York, and the coasts of CT, RI, and MA. We will hear what it was like to be a forecaster in the New York City (Upton) National Weather Service Forecast Office. We will again hear from the local Emergency Management Director of East Haven, CT. He spoke at the last weather conference about how his town survived Tropical Storm Irene. On the day of the conference, he had to leave to help evacuate his town for Sandy – he will compare and contrast the two storms. A TV meteorologist from Ocean City will share his views about the Sandy warning process and why he feels that many along the Jersey shore were unprepared. The Meteorologist In-Charge of the Taunton, MA Forecast Office will show storm survey images of damage along the Rhode Island coastline that resulted from Sandy.