Spotter Training 2004 - PowerPoint PPT Presentation

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Spotter Training 2004

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Spotter Training 2004 – PowerPoint PPT presentation

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Title: Spotter Training 2004


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May 22, 2004A date that was unforgettable
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May 22, 2004A date that was unforgettable
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It does not always look like a tornado!
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It does not always look like a tornado!
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54 miles long, 2.5 miles wideF4
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Lincoln
Bennet
Hallam
Daykin
Beatrice
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The Hallam Tornado
  • The storm did not look like a tornado to spotters
    and chasers. The fact that the cloud base was
    very low, the tornado circulation was very wide,
    along with the tornado being rain-wrapped at
    times, and darkness setting in made the storm
    extremely difficult to identify.

10
Reporting Procedures
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What do you report ?
  • Tornado or Funnel Cloud
  • Wall Cloud (rotation or rapid vertical motion?)
  • Hail (estimate size)
  • Wind Damage (estimate speed)
  • Shelf or Roll Clouds
  • Flash/Urban Flooding

12
HAIL SIZES
  • 1/4" PEA
  • 1/ 2" MARBLE ....TRY TO AVOID THIS
    DESCRIPTION
  • 3/4" DIME OR PENNY
  • 1" QUARTER
  • 1 1/4" HALF DOLLAR
  • 1 3/4" GOLFBALL
  • 2 1/ 2" TENNIS BALL
  • 2 3/4" BASEBALL
  • 3" TEACUP
  • 4" GRAPEFRUIT
  • 4 1/ 2" SOFTBALL

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How do you report ?Be ready to answer the
following questions
  • Who ?
  • What ?
  • When ? (Give time of event, not the current
    time)
  • Where ? (Give location, intersection of roads,
    GPS location, etc.)
  • Any damage from the event?

14
How to contact NWS with a report
  • Call law enforcement or dispatcher
  • Use amateur radio net
  • Use E-spotter
  • Toll free number

15
E-spotter is a NWS program that allows
spotters to email reports directly to the NWS
office. Spotter reports come directly into the
NWS AWIPS workstation and a local storm report
can be generated from these reports. To
register go to espotter.weather.gov
16
Hazardous Weather Outlook
  • Issued between 5 and 6 AM
  • Updated between 11 AM and NOON (April-Sept.) and
    between 5 and 6 PM or when needed
  • Discussion provides timing, location, coverage,
    probability and expected severity of weather

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Required Ingredients for Severe Thunderstorms
  • MOISTURE
  • Preferably in the lower or middle levels of the
    atmosphere
  • INSTABILITY
  • Ability for air to accelerate upward/downward
    when started up/down
  • SOURCE OF LIFT
  • Agent which lifts moist unstable air, starting
    the thunderstorm
  • WIND SHEAR
  • Winds that turn clockwise and/or increase in
    speed with height.

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Three Thunderstorm Stages
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Thunderstorm Classifications
  • Single Cell
  • Multicell Clusters
  • Multicell Lines (Squall Lines)
  • Supercell

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Supercell Thunderstorms
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Supercell Structure
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Radar View of Supercell
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Upper Level Storm Clues
Overshooting Top- Domelike bubble of cloud
material extending above the anvil and persisting
for gt 10 minutes
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Upper Level Storm Clues
  • Anvil Characteristics
  • Thick, cumuliform anvil with sharp,well-defined
    edges and backsheared

28
Video of a Supercell
29
Mid Level Storm Clues
A vertical and solid appearance to the main
updraft tower
30
Low Level Storm Clues
  • Rain-Free Base-
  • Low, flat cloud base with little visible
    precipitation falling and updraft towers above
  • Flanking Line -Row of towering cumulus stair-
    stepping up to main storm tower

31
MESOCYCLONES
  • A mesocyclone is the rotating updraft portion of
    a supercell storm.

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WALL CLOUDS
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A wall cloud is an isolated lowering of a
rain-free cloud base, usually underneath the most
intense part of the updraft, and attached to the
cloud base
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Tornado Life Cycle
  • Developing stage - Circulation associated with
    the funnel cloud descends to the ground and
    intensifies. Visible funnel increases in size.
  • Mature stage - Tornado reaches maximum size and
    intensity.
  • Rope stage - Tornado weakens and decreases in
    size.

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Developing Tornado
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Fast Developing Tornado
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Mature Tornado
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Mature Tornado
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Rope Stage Tornado
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Tornado from Development to Rope Stage
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Other Thunderstorm Hazardsand Safety
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Lightning is the spotters most common danger!
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Damaging Winds
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Rear Flank Downdraft
  • The rear flank downdraft or RFD can be very
    intense. Spotters should stay a safe distance
    from the wall cloud and tornado

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Strong or damaging winds can occur right along
the leading edge of the shelf cloud
  • Photo by Marty Feely near Missouri Valley

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Scud
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WALL CLOUDS SHELF CLOUDS
  • SUGGEST INFLOW/UPDRAFT
    SUGGESTDOWNDRAFT/OUTFLOW
  • MAINTAIN POSITION WITH MAY
    MOVE AWAY FROM THE
  • RESPECT TO THE UPDRAFT STORM
    IN THE DOWNDRAFT

  • REGION
  • ROTATE ABOUT A VERTICAL MAY
    ROTATE ABOUT A
  • AXIS
    HORIZONTAL AXIS

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Flash Floods
Lincoln, NE August 28, 2002
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Two unusual deaths attributed to heavy rainfall
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Make sure you pay attention to the signs
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Do not get too close!
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Avoid getting caught in the heaviest
precipitation area north of the mesocyclone or
the Bears Cage THIS AREA HAS THE LARGEST
HAIL!
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Spotter Safety
  • Be alert to hazardous driving conditions like wet
    roads and poor visibility
  • Avoid distractions while driving such as
    Operating radios or cell phones or watching
    storms
  • Always have an escape route
  • Stay in your vehicle as much as possible because
    of lightning and large hail
  • Do not hide under an overpass!

63
Night Spotting
Lightning illuminates cloud features or look for
flashes of light from power lines or transformers.
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Final thoughts..
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How many minutes is your county under a tornado
warning each year?
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Killer Tornadoes 1950-2003
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NATIONAL WEATHER SERVICE WEB SITE
  • www.crh.noaa.gov/oax/
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