1993-Present

 

Hit Counter
hits

 

 

 

CURRENT WEATHER DATA



 

Strom Prediction Center - Mesoscale Discussion

 

Watches, Warnings and Advisories

 

 

Taunton, Massachusetts RADAR

with Clutter
without Clutter

 

Lightning Data-Thunderstorm Fcst

 

Storm Prediction Center Data, Norman, Oklahoma

 

Surface Maps

 

 

 

 

 

Eastern Mass. ARES/RACES/SKYWARN Links

 Eastern Mass. ARES/RACES/SKYWARN Index

 Amateur Radio SKYWARN Net Frequency List

 

What is SKYWARN?

    SKYWARN is a national network of volunteer severe weather spotters. The spotters are trained by local National Weather Forecast Offices on how to spot severe  thunderstorms, tornadoes, hail and flooding. In parts of the country, spotters also report snowfall and ice.

SKYWARN History

    During the early 1940's the Weather Bureau cooperated with the military in setting up volunteer spotter networks to protect military installations. After a tornado killed 80 and injured 273 people in Kansas in 1955,the Weather Bureau decided to train severe weather spotters. On March 8,1959, in Wellington, Kansas, the first training course for 225 severe weather spotters was held.

How does SKYWARN Amateur Radio work?

    Two-thirds of the volunteers are licensed amateur radio operators. Amateur radio plays a big role in the SKYWARN program. During severe  weather, amateur radio volunteers man a amateur radio station at the National Weather Service Office. They talk to the spotters in the particular area that the storm is occuring and request information needed by the forecasters. Large storms knock out phone service. SKYWARN amateur radio volunteers are there to relay severe weather reports to the national weather offices to keep communities informed of severe weather. The National Weather Service issues watches and warnings warnings, based in part on observations from storm spotters in the field. Your reports are important to warning forecasters who are making critical warning decisions.

How do I become a weather spotter?

    You must take a SKYWARN class. This class is a  free 3-hour  seminar that  teaches you  the basics of  how SKYWARN operates, how to spot severe  weather, what to report, how to report and when to report it. At the end of the class, you are given a special SKYWARN ID card with reporting instructions. There is no cost for the class. SKYWARN Training classes are held each spring.

What Spotters Look For

    Storm spotters play a vital role in the warning and information process by observing storms and making reports back to the National Weather Service and local public safety officials. Trained spotters learn about the physical structure of severe storms and how to identify the most likely areas for severe weather development. They also learn about visual clues that may precede tornado development, and learn to distinguish between real tornadoes and look-alikes. These types of details, when coupled with NWS forecasters’ expert radar interpretation, lead to better warnings and statements. Once SKYWARN Spotter observation reports are received by the National Weather Service office via a toll-free 800 number or web email, the reports are sent to the media (i.e., Weather Channel, etc..)

-----------------------------

SKYWARN Reporting Criteria

How to report

When making a report, remember to answer three basic questions...

WHAT Happened? Type of Event (Tornado, downed trees, etc..)
WHEN did the event happen? Also, duration of the event.
WHERE did the event happen? Location of event (town or city, portion of county, major intersections)

What To Report

Tornadoes
Funnel Clouds and Wall Clouds
Rotating Thunderstorms
Wind Gusts Greater Than 45 mph
Hail (any size)
Wind Damage
Flooding
Heavy Rain
Power Outages
Any weather related deaths and injuries

---------------------------------------

Spotters Safety Tips

Safety should be first and foremost on the mind of a spotter. Remember, the N.W.S. values your safety more than your observations. It is essential that spotters proceed into the field armed not only with knowledge of the storms but also with an understanding of the dangers posed by thunderstorms. When spotting, travel in pairs if at all possible. When moving, this will allow the driver to remain focused on the chore of driving while the passenger keeps an eye on the sky and handles any communication with the dispatcher. When stopped, two sets of eyes are available for observation.

      Keep aware of the local environment at all times. When in the vicinity of a thunderstorm, keep a 2-mile "buffer zone" between you and the storm. Frequently check the sky overhead and behind to ensure no unexpected events (such as a new tornado) are developing. Always have an escape route available, in case threatening weather approaches or if you get within the 2-mile "buffer zone."

      Lightning is the number one killer among weather phenomena. During a typical year, lightning kills more people than hurricanes, tornadoes, and winter storms combined. The two main threats posed by lightning are the intense heat of the lightning stroke (about 15,000 degrees Celsius) and the extreme current associated with the stroke, estimated at 30,000 amperes (less than 1 ampere can be fatal).

      Lightning is also the biggest weather hazard facing the spotter. When in the field, the spotter will usually be in a preferred lightning strike area (in the open, on a hilltop, etc.). Whenever possible, remain in your spotting vehicle to minimize the chance of being struck by lightning. If you must leave your vehicle, crouch as low as possible to make yourself a less favorable target. Hail is usually not a direct threat to life, but hailstorms are the costliest weather element to affect the United States. Each year, hailstorms cause over $1 billion in damage primarily to crops, livestock, and roofs. Giant hailstones (2 inches or more in diameter) can reach speeds of 100 miles an hour as they fall to earth. If such a stone strikes someone, the results can be fatal. There have been only two documented hail related deaths in the United States, but a hailstorm in China killed over 100 people in 1976. A vehicle will usually offer adequate protection from moderate sized hailstones. Hail larger than golf ball size may damage windshields, so avoid large hail shafts if at all possible.

      Down bursts are underrated thunderstorm threats. A down burst is defined as a strong down draft with an out rush of damaging winds on or near the earth's surface. Down bursts are responsible for the "wind shear" which has caused a number of airliner accidents in the 1970's and early 1980's. When people experience property damage from a down burst, they often do not believe that "just wind" could have caused the damage, and they assume that they were struck by a tornado. In fact, the strongest down bursts have wind gusts to near 130 miles an hour and are capable of the same damage as a medium sized tornado.

      Down bursts are classified based on their size. If the swath of damaging winds is 2.5 miles or greater, it is called a macroburst. If the swath is less than 2.5 miles across, it is called a microburst. In general, macrobursts are long-term, large scale events, while microbursts are intense, quick hitting phenomena. Microbursts are subdivided as wet or dry microbursts, depending on how much rain falls with the microburst. If very heavy rain falls with the microburst, it is called a wet microburst, while a dry microburst has little or no rain reaching the ground.

      Flash floods are another example of an underrated thunderstorm threat. Over the past several years, more people have been killed in flash floods than in tornadoes. Two factors are responsible for this. First, we have urbanized. Where rain water used to have open fields in which to run off, it now has highway intersections, basements, streets, etc. Second, the public as a whole is apathetic about flash flooding. We simply do not treat flash flooding with the respect it deserves. Many of the recent deaths associated with flash flooding have occurred because people attempted to drive their vehicles across a flooded low water crossing and were swept away by the flood waters. Less than two feet of moving water is needed for a vehicle to be swept away. When spotting in a flash flood situation, follow these common sense safety tips. Remember that flash flooding is most dangerous at night when the effects of flash flooding are difficult to see. Since most flash floods occur at night, this problem is compounded. Avoid low water crossings and don't drive into areas where water covers the road. If you are caught in a flash flood, abandon your vehicle and quickly get to higher ground.

      Last but not least is the tornado. Again, a tornado is defined as a violently rotating column of air in contact with the ground and pendant from a thunderstorm (whether or not a condensation funnel is visible to the ground). If the violently rotating column of air has not touched the ground, it is called a funnel cloud. If a tornado is approaching your location, drive away from the tornado IF you are in open country, IF the location and motion of the tornado are known, and IF you are familiar with the local road network. If you are in an urban area and escape is not possible for some reason, abandon your vehicle and get into a reinforced building. If a reinforced building is not available, get into a culvert, ditch, or other low spot in the ground (that is not flooded).

      Spotting at night is obviously more difficult than spotting during the day. There are only a few allies available to help you when night spotting. If possible, use the light from lightning flashes to illuminate the important parts of the storm. Quite often, though, lightning strokes will be very brief and will illuminate different parts of the storm from different angles. This will make it even more difficult to accurately report what is occurring. If you are in large hail, the most dangerous part of the storm is near you and will probably move overhead within a few minutes. If you hear a loud roaring sound, then a tornado may be very close to your location. Use this tip with caution. Not all tornadoes have a loud roar, and some non-tornadic winds may also possess a loud roar. Finally, if you think there is a tornado not far from your location (i.e., within spotting range), search along the horizon for bright flashes of light as the tornado destroys power lines and transformers.

---------------------------------------

What is RACES?

    The Radio Amateur Civil Emergency Service (RACES), is a public service provided by a reserve volunteer group of Amateur Radio Operators that is administered by local, county and state emergency management agencies, and supported by the Federal Emergency Management Agency (FEMA) of the United States government. As a part of the Amateur Radio Service, it provides radio communications for civil-preparedness purposes only, during periods of local, regional or national civil emergencies. These emergencies are not limited to war-related activities, but can include natural disasters such as earthquakes, hurricanes, wildfires, power outages, floods, victim searches, air crashes, and many others.

 

What is ARES?

    The Amateur Radio Emergency Service (ARES) consists of licensed amateurs who have voluntarily registered their qualifications and equipment for communications duty in the public service when disaster strikes. Every licensed amateur, regardless of membership in ARRL or any other local or national organization, is eligible for membership in the ARES. The only qualification, other than the possession of an Amateur Radio license, is a sincere desire to serve. Because ARES is an amateur service, only amateurs are eligible for membership. The possession of emergency-powered equipment is desirable, but is not a requirement for membership.

    The Taunton, Massachusetts National Weather Service has a SKYWARN / ARES Spotting Program. The amateur radio call is WX1BOX. SKYWARN Spotters and amateur radio operators send reports to the weather service ops via phone or radio communication. There are many frequencies where the SKYWARN weather nets are run. Most are on the 2 meter (144-148 MHz) and 70 centimeter ( 420-450 MHz) bands.

The Southeast Massachusetts Weather Net Schedule

The Cape Cod and Islands Weather Net, 146.955 MHz Barnstable Repeater
       Monday-Friday 6:00-6:30 am.
The Fairhaven Weather Net, 145.490 MHz Fairhaven Repeater
       Monday-Friday 8:00-8:30 pm.
The SKYWARN Rhode Island Weather Net, 146.760 MHz Cranston Repeater
       Wednesday Evenings at  8:30 pm
The National Hurricane Net, 14.325 MHz (Upper Side Band) Seasonal Broadcasts

 

 Amateur Radio Repeater and NOAA Weather Frequencies

Massachusetts / Rhode Island Amateur Radio Repeaters...

>>> Massachusetts....Dennis 146.955 pl: 88.5 hz.....Falmouth 146.655.....Fair Haven 145.490.....Bridgewater 147.180.....Walpole 146.845.....Waltham/Boston 146.640.....Danvers 145.470 pl: 136.5 hz.....Mt. Tom 146.940.....Worcester 146.925 pl: 100 hz.....Haverhill 146.625.....In Rhode Island  Statewide 146.760.....Cranston 146.700.......The National Hurricane Net...14.325 (usb mode).......    

NOAA Weather Radio Broadcasts...

>>>Falmouth/Cape Cod 162.550.....Boston 162.475....Glouster 162.425....Worcester 162.550....Mt. Greylock 162.525....Somers,Ct. 162.475.....Peterborough,NH 162.525....in Rhode Island 162.400<<<

NOAA Weather Radio
LISTEN LIVE
Albany, N.Y.
Boston, Ma.
Hartford, Ct.
Holderness, NH.
Pack Monadnock, N.H.
Providence, R.I.

 

 

Weather Tools

Clouds

High clouds above 18,000 feet are cirrus clouds.

  Cirrus clouds are the most common of the high clouds. They are composed of ice and consist of long, thin, wispy streamers. Cirrus clouds are usually white and predict fair weather. Sometimes called mares tails, they stream with the wind. By watching the movement of cirrus clouds you can tell from which direction weather is approaching. The appearance of cirrus clouds usually indicates that a change in weather will occur within 24 hours.
   Cirrostratus are sheet-like, thin clouds that usually cover the entire sky. The sun or moon can shine through Cirrostratus clouds. Cirrostratus clouds usually come 12-24 hours before a rain or snow storm.
   Cirrocumulus are small, rounded puffs that usually appear in long rows. They are usually white, but sometimes appear gray. Cirrocumulus are usually seen in the winter and indicate fair, but cold, weather. In the tropics, they may indicate an approaching hurricane.

Medium high clouds occupy altitudes of 6,500 feet to 18,000 feet

    An Altostratus cloud usually covers the whole sky. The cloud looks gray or blue-gray. The sun or moon may shine through an Altostratus cloud, but will appear hazy. An altostratus cloud usually forms ahead of storms with continuous rain or snow.

    Altocumulus clouds are grayish-white with one part of the cloud darker than the other. Altocumulus clouds usually form in groups. If you see Altocumulus clouds on a warm, sticky morning, be prepared for thunderstorms by late afternoon.

Low clouds, called stratus clouds, are at altitudes up to 6,500 feet

   Stratus clouds are uniform gray in color and almost cover the entire sky. Light mist or drizzle is sometimes associated with Stratus clouds. A Stratus cloud touching the ground is fog.