Title: Spotter Training 2004
1(No Transcript)
2May 22, 2004A date that was unforgettable
3May 22, 2004A date that was unforgettable
4It does not always look like a tornado!
5It does not always look like a tornado!
6(No Transcript)
754 miles long, 2.5 miles wideF4
8Lincoln
Bennet
Hallam
Daykin
Beatrice
9The 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.
10Reporting Procedures
11What 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
12HAIL 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
13How 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?
14How 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
16Hazardous 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
17(No Transcript)
18Required 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.
19Three Thunderstorm Stages
20Thunderstorm Classifications
- Single Cell
- Multicell Clusters
- Multicell Lines (Squall Lines)
- Supercell
21Supercell Thunderstorms
22(No Transcript)
23Supercell Structure
24(No Transcript)
25Radar View of Supercell
26Upper Level Storm Clues
Overshooting Top- Domelike bubble of cloud
material extending above the anvil and persisting
for gt 10 minutes
27Upper Level Storm Clues
- Anvil Characteristics
- Thick, cumuliform anvil with sharp,well-defined
edges and backsheared
28Video of a Supercell
29Mid Level Storm Clues
A vertical and solid appearance to the main
updraft tower
30Low 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
31MESOCYCLONES
- A mesocyclone is the rotating updraft portion of
a supercell storm.
32(No Transcript)
33WALL CLOUDS
34A 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
35(No Transcript)
36(No Transcript)
37Tornado 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.
38Developing Tornado
39Fast Developing Tornado
40Mature Tornado
41Mature Tornado
42Rope Stage Tornado
43Tornado from Development to Rope Stage
44(No Transcript)
45Other Thunderstorm Hazardsand Safety
46Lightning is the spotters most common danger!
47 Damaging Winds
48Rear Flank Downdraft
- The rear flank downdraft or RFD can be very
intense. Spotters should stay a safe distance
from the wall cloud and tornado
49(No Transcript)
50Strong or damaging winds can occur right along
the leading edge of the shelf cloud
- Photo by Marty Feely near Missouri Valley
51(No Transcript)
52(No Transcript)
53Scud
54WALL 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 -
55(No Transcript)
56Flash Floods
Lincoln, NE August 28, 2002
57Two unusual deaths attributed to heavy rainfall
58Make sure you pay attention to the signs
59Do not get too close!
60Avoid getting caught in the heaviest
precipitation area north of the mesocyclone or
the Bears Cage THIS AREA HAS THE LARGEST
HAIL!
61(No Transcript)
62Spotter 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!
63Night Spotting
Lightning illuminates cloud features or look for
flashes of light from power lines or transformers.
64(No Transcript)
65Final thoughts..
66How many minutes is your county under a tornado
warning each year?
67Killer Tornadoes 1950-2003
68NATIONAL WEATHER SERVICE WEB SITE