SOUTH SHORE SKYWARN GROUP
South Eastern Massachusetts
SKYWARN
OBSERVER'S GUIDE
REVISED 09/24/99
Safety Precautions!
When acting as a spotter, always remember that your safety is most important. During a thunderstorm with lightning, stay in your covered vehicle with the windows up and door shut.
Do not try to outrun a tornado in your car. Get out of your car and curl up into a ball in a ditch or ravine in a location that will be as free of flying debris as you can, but be aware of localized flooding. Keep your head covered and eyes closed.
Above all else, use common sense and dont take unnecessary risks.
Please include the following items in all your SKYWARN reports:
WHAT: Describe event.
WHERE: Direction, and distance from known location, plus movement, and speed of condition being observed.
WHEN: EXACT time of event.
BY WHOM: Spotter name (plus callsign if Ham radio operator), and location.
WHAT TO REPORT
ONLY REPORT
OBSERVATIONS,
NOT INTERPRETATIONS!!!
- Report time of observation
- Location
- Direction of motion
- Report time of observation
- Location
- Estimated wind speed
- Estimated wind direction
- Report time of observation
- Location
- Size of hailstones -- Measure if possible, report largest size, most common size, and depth of coverage. For size reference use pea, marble, dime, quarter, golfball, baseball, softball.
- Report time of strike
- Location
- What was struck
- If a person was struck, report what person was doing, age, & sex
- Report time of observation
- Location
- Depth of standing water (if possible)
- Actual rainfall rate (if possible)
Always record and report the time of your observation
Always identify yourself
If a SKYWARN net has been activated in your County then report your observations to your Net Control Station.
If no SKYWARN net has been activated in your area, then you may report your observations on the District SKYWARN frequency, or by phone to your local emergency management office, law enforcement agency, or the National Weather Service.
The GENERAL PUBLIC should contact their local law enforcement agency during times of severe weather, NOT the National Weather Service.
Notes:
When spotting for wall clouds, funnel clouds, tornadoes, and waterspouts the key is always to look for rotation! Often, scud clouds are mistaken for funnels or tornadoes because they may form beneath the parent thunderstorm and appear to touch the ground. Just remember... with scud there will be no rotation.
When estimating wind speed feel free to use the Beaufort Wind Scale provided in this guide (condensed below). Study the description of the Effects Observed and choose the appropriate wind speed range from the table. Report the speed in miles per hour or in knots. DO NOT REPORT THE BEAUFORT FORCE NUMBER. This will likely send the meteorologists at the National Weather Service scurrying for reference books, wasting valuable time.
ESTIMATING WIND SPEED
25-31 - Large branches moving. Whistling in overhead wires.
32-38 - Whole trees moving. Inconvenience in walking against wind.
39-46 - Small branches (twigs) break. Impedes walking.
46-54 - Slight structural damage. Larger branches, and weak limbs may break.
55-63 - Moderate structural and tree damage.
64 and above - Heavy to severe tree, and structural damage.
When reporting wind direction remember that meteorologists always do things backwards. The wind direction reported is ALWAYS the direction from which the wind is blowing. For example, if you report the winds as Southerly at 10 mph, that means the winds are coming from the south blowing to the north.
When reporting hail, use the common references that are used by the National Weather Service. That is, describe them as pea-sized (1/4 inch), marble-sized (1/2 inch), dime-sized (3/4 inch), quarter-sized (1 inch), golfball-sized (1 3/4 inch), baseball-sized (2 3/4 inch) (arggghhhh... lets hope you never have to report that)!!!
When assessing wind damage, remember that most wind damage is done by straight-line winds, not by tornadoes. With straight-line wind damage, all the damage will look like it diverges (moves outwards) from a single point possibly in several directions. With tornado damage, destruction is generally along one direction, debris along the ground is twisted or has spiral characteristics, and often small arcs where the top-soil has been removed are visible.
If a person is struck by lightning take appropriate action to ensure immediate aid is given. A person retains no electrical charge after being struck, so it is safe to touch that person. This means CPR can be administered immediately if necessary.
1. Always have a safe place nearby to protect yourself from wind and/or hail.
2. Cars are a safe place from lightning, but NOT from tornadoes.
3. Moving water is powerful, it only takes a slight current to push a vehicle off the road.
4. Large hail often falls just in advance of a tornado, especially large ones.
5. Tornadoes generally move toward the NORTHEAST at 25 to 35 MPH when associated with fronts, and squall lines but CAN travel at 70 MPH.
6. The first gust of wind to reach you from a thunderstorm is frequently the strongest.
7. WALL CLOUDS form on the rain free base often 15 to 20 minutes before the tornado occurs.
8. A rain free base denotes the storm's updraft area, a place to watch closely.
9. Overshooting tops are an indicator of a very strong storm.
TORNADOES usually form in the trailing edge of a thunderstorm. Wind speeds can reach 300 MPH in "MAXI" TORNADOES. Conventional radar can't see a tornado... it only sees the rain, and hail.
Thanks to the Internet you can participate in Project Verify (NSSL Severe Weather Reports Database). To help NWS/NSSL fine tune the 88D radars they need information about Tornadoes, Hail, Thunderstorm Winds and Thunderstorms. For more information click here.
The Spotters Observation Kit
Consider keeping the following equipment handy:
Weather radio (Its nice to be able to keep up with weather warnings.)
Communications radio for reporting your observations (When you see severe weather, youve got to report it!)
Raincoat with hood (Stay dry!)
Flashlight (In case you cant see when it gets dark!)
Binoculars (So you can tell whether that cloud is really rotating!)
Camera or Camcorder (So that a permanent record can be made of your observations. Pictures and video are the BEST form of training for other spotters.)
Compass (For estimating the wind direction -- remember...thats the direction the wind is coming from!)
Your SKYWARN Observers Guide (So you can remember all this stuff!)
Some Meteorological Terms
ANVIL
The top portion of a mature thunderstorm that has the appearance of having been "blown off".
ARC CLOUD
Also sometimes called a shelf cloud. This is usually the dark, ominous looking cloud formation the precedes the passage of a squall line or multicell thunderstorm formation. It is formed as warm moist air overrides cool downdraft winds at the leading edge of the thunderstorm (the gust front).
CELL
The basic thunderstorm, which consists of one updraft and one downdraft.
DEBRIS CLOUD
Area of dust, sand, and debris that forms near the ground at the base of a tornado.
DOWNBURST
A small area of rapidly descending air beneath a thunderstorm. Downburst winds hit the ground and spread out, often at speeds in excess of 100 mph. See also downdraft, macroburst and microburst.
DOWNDRAFT
Area within a thunderstorm where the predominant air motion is downward. Where there is precipitation there will always be a downdraft. Downbursts are localized areas within the downdraft of very rapidly descending air.
FUNNEL (CLOUD)
Generally the funnel is a visible tornado that hasnt yet reached the ground. Funnels consist of water droplets that have condensed due to the rapid temperature and pressure changes in the vicinity. Also called condensation funnel.
GUST FRONT
The area near the leading edge of a thunderstorm where downdraft winds hit the earths surface and spread out. The gust front is the leading edge of the spreading winds. The gust front is usually found just below or very near the arc cloud.
HAIL
Large ice chunks that grow within the thunderstorm until they are too heavy to be supported by the mechanics within the storm. Large hailstones fall at speeds greater than 100 mph.
INFLOW
Area of a thunderstorm where air from the surrounding environment is "sucked up" into the thunderstorm updraft. The inflow area is always void of precipitation and the cloud bases are dark and flat.
MACROBURST
A downburst with a diameter of greater than 2.5 miles.
MAMMATUS
Downward protruding "bumps" usually on the underside of the anvil of a thunderstorm. Mammatus ("Mama") clouds are indicative of extreme turbulence.
MICROBURST
A downburst with a diameter of 2.5 miles or less.
OUTFLOW
That portion of the thunderstorm where the downdraft winds hit the surface of the earth and spread out.
OVERSHOOTING TOP
A protruding cloud area above the usually smooth anvil of a mature thunderstorm that indicates the presence of an intense updraft.
SCUD (CLOUD)
Clouds that appear to have broken off beneath the base of a thunderstorm. Scud (fractus) clouds often may reach to near the ground and can be easily mistaken for a funnel.
SHELF CLOUD
See Arc Cloud.
TAIL CLOUD
Scud-type cloud that forms near the base of a wall cloud and protrudes almost parallel to the earth toward the main precipitation shaft of the thunderstorm.
TORNADO
Rotating area of strong winds and rapid pressure change that sometimes forms in conjunction with a severe thunderstorm.
UPDRAFT
The area within the thunderstorm where the predominant air motion is upward.
VAULT
An area of dry clear air that often forms between the main precipitation shaft and the rain-free base wall cloud.
WALL CLOUD
A rotating cloud that forms beneath the base of the thunderstorm behind the main precipitation shaft where some of the inflowing air and outflowing air meet and mix. Tornadoes, if they occur, will appear to drop out of the wall cloud.
WATERSPOUT
A weak tornado that forms over warm water. The formation mechanisms for waterspouts are different from those of land tornadoes, and waterspouts may form during relatively calm-looking weather
BEAUFORT WIND SCALE |
|||||
Beaufort |
Wind Speed |
NWS |
Effects Observed |
Effects Observed |
|
mph |
knots |
||||
0 |
< 1 |
< 1 |
Calm | Calm; smoke rises vertically | Sea like mirror |
1 |
1 - 3 |
1 - 3 |
Light air | Direction of wind shown by smoke drift, but not by wind vanes | Ripples with scaly appearance; no foam crests |
2 |
4 - 7 |
4 - 6 |
Light breeze | Wind felt on face; leaves rustle; ordinary vane moved by wind | Small wavelets, crests of glassy appearance and not breaking |
3 |
8 - 12 |
7 - 10 |
Gentle breeze | Leaves and small twigs in constant motion; wind extends light flag | Large wavelets with crests beginning to break, scattered whitecaps |
4 |
13 - 18 |
11 - 16 |
Moderate breeze | Raises dust and loose paper; small branches are moved | Small waves growing larger, numerous whitecaps |
5 |
19 - 24 |
17 - 21 |
Fresh breeze | Small trees in leaf begin to sway; crested wavelets form on inland waters | Moderate waves with greater length, many whitecaps with some spray |
6 |
25 - 31 |
22 - 27 |
Strong breeze | Large branches in motion; whistling heard in telegraph wires; umbrellas used with difficulty | Larger waves, whitecaps very numerous, more spray |
7 |
32 - 38 |
28 - 33 |
Near gale | Whole trees in motion; resistance felt in walking against wind | Sea tends to heap up, streaks of foam blown from breaking waves |
8 |
39 - 46 |
34 - 40 |
Gale | Breaks twigs off trees; generally impedes progress | Fairly high waves of greater length, well-marked streaks of foam |
9 |
47 - 54 |
41 - 47 |
Strong gale | Slight structural damage occurs (chimney pots and slate removed) | High waves with sea beginning to roll, dense streaks of foam with spray blown higher into air--may cut visibility |
10 |
55 - 63 |
48 - 55 |
Storm | Trees uprooted; considerable structural damage occurs | Very high waves with overhanging crests, sea is white with foam, heavy rolling and reduced visibility |
11 |
64 - 72 |
56 - 63 |
Violent storm | Widespread structural damage | Waves exceptionally high, sea covered with foam, visibility further reduced |
12 |
73 - 82 |
64 - 71 |
Hurricane | Maximum wind damage | Sea completely covered with spray, air filled with foam, greatly reducing visibility |
13 |
83 - 92 |
72 - 80 |
|||
14 |
93 - 103 |
81 - 89 |
|||
15 |
104 - 114 |
90 - 99 |
|||
16 |
115 - 125 |
100 - 108 |
|||
17 |
> 125 |
> 108 |
Source: Meteorology, William L. Donn, 1975,
McGraw-Hill, Inc., New York.
FUJITA SCALE FOR TORNADO INTENSITY |
||||
scale |
category |
mph |
knots |
expected damage |
F - 0 |
WEAK |
40 - 72 |
35 - 62 |
light: tree branches broken, sign boards damaged |
F - 1 |
73 - 112 |
63 - 97 |
moderate: trees snapped, windows broken | |
F - 2 |
STRONG |
113 - 157 |
98 - 136 |
considerable: large trees uprooted, weak structures destroyed |
F - 3 |
158 - 206 |
137 - 179 |
severe: trees leveled, cars overturned, walls removed from buildings | |
F - 4 |
VIOLENT |
207 - 260 |
180 - 226 |
devastating: frame houses destroyed |
F - 5 |
261 - 318 |
227 - 276 |
incredible: structures the size of autos moved over 100 meters, steel reinforced structures highly damaged |
Source: Meteorology Today, C. Donald Ahrens,
1991, West Publishing Company, St. Paul.
SPOTTER TRAINING WEB SITES:
Introduction To Observation Weather TechniquesNOAA Severe Storms Spotter Guide Online
Severe Weather Safety - NWSFO Norman, OK
Spotter Guide - NWSFO Norman, OK
Cloud Boutique - PSC Meteorology Program
Selected Internet Resources For The Beginning Storm Chaser
Storm Spotters Guide - Guide To Meteorology (UIUC)
Storm Track's Storm Chase Guide
Weather Glossary For Storm Spotters
The Forecast Factory
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