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Home My WebLink About04 BCCD Minutes and Attachments 04.10.1990 BRAZOS H n O�P COUNTY Mary Kaye Moore JAKE CANGLOSE lMARVINNORWOOo- COORDINATOR & CHAIRMAN INTER - JURISDICTIONAL OFFICE BRYAN COORDINATOR E.E. BURNS CIVIL DEFENSE & EMERGENCY PLANNING COUNTY COURTHOUSE COUNTY DEPUTY COORDINATOR HARRY STITELER TAMU COORDINATOR BRYAN, TEXAS 77803 STEVE BEACHY COLLEGE STATION COORDINATOR MEETING AGENDA APRIL 10, 1990 I. REVIEW AND APPROVAL OF SEVERE WEATHER BASIC PROCEDURES Bryan Police Department Brazos County Sheriff Office College Station Police Dept. Department of Public Safety Texas A&M University Police II. RADIO /TELEVISION STATION COORDINATION KBTX -TV WTAW -AM KAGG -FM KAMU -TV & FM KTSR -FM TCA Cablevision KORA -FM KKYS -FM KTAM -AM KWBC -AM KAGC -AM KNAV -FM III. A. IMPROVEMENT OF TELEVISION /RADIO NOTIFICATION TIME FROM LOCAL AUTHORITIES ON ADVISORIES, WARNINGS, AND EMERGENCY MESSAGES (i.e. EVACUATIONS, ETC.) B. FUTURE CENTRAL DISPATCH PROCEDURES IV. STORM SPOTTERS PROCEDURES AND REVIEW V. OTHER BRAZOS COUNTY BRYAN COLLEGE STATION TEXAS A &M UNIVERSITY BRAZOS F c m1 COUNTY Mary Kaye Moore JAKE CANGLOSE - ARVFN NORWOOD COORDINATOR & CHAIRMAN INTER- JURISDICTIONAL OFFICE BRYAN COORDINATOR CIVIL DEFENSE & EMERGENCY PLANNING E.E. BURNS HARRY STITELER COUNTY DEPUTY COORDINATOR COUNTY COURTHOUSE TAMU COORDINATOR BRYAN, TEXAS 77803 STEVE BEACHY COLLEGE STATION COORDINATOR SEVERE WEATHER REPORTING AND WARNING PROCEDURES I. LAW ENFORCEMENT AGENCIES RESPONSIBILITIES (Area of Jurisdiction) 1. TORNADO OR FUNNEL CLOUD REPORTS Dispatcher will; a. Send nearest unit to reported area immediately for confirmation and determination of other emergency units needed such as fire, ambulance, etc. b. Notify County Emergency Management /Civil Defense Coordinator at 846 -7428 as well as City Emergency Management Coordinator. c. Coordinate assistance requests and follow internal notification procedures. d. Notify radio /TV stations to broadcast warnings or special advisories when directed by proper authority. e. Notify D.P.S. on all confirmed severe weather reports. f. Maintain records on all weather incident reports. 2. SEVERE WEATHER REPORTS (High Winds - -58 mph or higher- - Hail--3/4", dime -size or larger- - or Road Flooding) Dispatcher will; a. Send nearest unit to area for confirmation and report conditions to D.P.S., your County Emergency Management/ Civil Defense Coordinator (846- 7428), and your City Emergency Management Coordinator. b. Notify officials and agencies as outlined in internal notification procedures. BRAZOS COUNTY BRYAN COLLEGE STATION TEXAS A &M UNIVERSITY -2- II. LOCAL DEPARTMENT OF PUBLIC SAFETY RESPONSIBILITIES a. Forward all tornado and severe weather reports to Waco NWS and coordinate with County Emergency Management/ Civil Defense Coordinator. b. In the event of major disaster, dispatch a unit to disaster area. c. Coordinate with local officials on all local area severe weather reports received or severe weather spotted. d. Disseminate on teletype severe weather advisories or warnings issued by local authority. III. RADIO AND TELEVISION STATION RESPONSIBILITIES a. Upon receipt of public reports of tornado or severe thunderstorms, immediately notify law enforcement dispatcher in area of jurisdiction and County Emergency Management /Civil Defense Coordinator (846- 7428). b. When notified by local Emergency Management /Civil Defense, Police Departments, Sheriff's Office, or D.P.S., BROADCAST IMMEDIATELY Warnings or Severe Weather Advisories. NOTE: Local warnings and severe weather advisories must be preceded with or ended by: Authority Brazos County Emergency Management /Civil Defense Coordinator and use statement as given. c. Broadcast all National Weather Service Watches, Warnings. and Special Weather Bulletins issued for the local area. TORNADO AND SEVERE WEATHER SPOTTING PROCEDURES TORNADO REPORTING 1 . IDENTIFY YOURSELF. If you are at a telephone, give your number, exact location or street address. 2 . REPORT WHETHER THE FUNNEL IS ON THE GROUND OR ALOFT. 3 . TORNADO LOCATION - BE AS ACCURATE AS POSSIBLE. 4 . GENERAL DIRECTION OF TRAVEL IF POSSIBLE. 5 . ESTIMATED SPEED OF TRAVEL IF POSSIBLE. 6. PROPERTY DAMAGE OR POSSIBLE INJURIES. If you have seen property damage, state so and whether or not you have reason to believe some one may be injured. REPORT A FUNNEL CLOUD ONLY IF YOU ARE SURE THIS IS WHAT YOU SEE. (Many cloud bases are ragged in ways that, when viewed from certain angles, make them appear to be tornadic. Look for cloud base rotation. KEEP YOUR STATION AS LONG AS YOU SAFELY CAN. IF YOU MUST LEAVE TO TAKE COVER, DO SO. IF YOU LOSE SIGHT OF THE VORTEX, ADVISE THE CENTER. REPORTING PROCEDURES 4S 16'( - 6 1. Call 846 - 7428,E or your local Law Enforcement Agency 2. Organized weather spotters — Report weather to your designated communication center. SEVERE WEATHER REPORTING: 1. REPORT HAIL (GIVE APPROXIMATE SIZE AND INTENSITY— 3/4" or larger, approx. dime size). 2. REPORT STRAIGHT LINE DAMAGING WINDS — 58 mph or higher (REPORT DAMAGE OBSERVED TO TREES & STRUCTURES). 3 . REPORT FLOODING CONDITIONS AND ROAD HAZARDS CAUSED BY SEVERE WEATHER. ESTIMATING WIND SPEEDS (miles per hour) 25 -31 Large branches in motion; whistling 55 -72 Damage to chimneys and TV heard in telephone wires. antenna; pushes over shallow rooted trees. 32 -38 Whole trees in motion; inconvenience 73- 112....Peels surface off roofs; felt walking against wind. windows broken; Tight trailer houses pushed or 39 -54 Twigs break off trees; wind generally overturned; moving auto - impedes progress. mobiles pushed off roads. NATIONAL WEATHER SERVICE STORM SPOTTER'S GLOSSARY AND SUPPLEMENTAL GUIDE ACCESSORY CLOUDS -- Clouds that are dependent on a larger cloud system for development and continuance. Accessory clouds associated with the thunder- storm include roll, shelf, mammatus, and wall clouds. ANVIL -- The spreading of the upper portion of a cumulonimbus cloud into an anvil- shaped plume usually of fibrous or smooth appearance. Strong or severe thunderstorms often have thicker anvils with the side and bottom having a cumuliform or slowly boiling appearance in the immediate vicinity of the parent cumulonimbus. COLLAR CLOUD -- Frequently used as a synonym for a wall cloud although it actually is a generally circular ring of cloud surrounding the upper portion of a wall cloud. CUMULONIMBUS CLOUD -- The parent cloud of a thunderstorm. The cumulonimbus cloud towers above ordinary cumulus clouds, with stronger or severe storms often having a more sharply outlined "hard" appearance with relatively rapid rising motions visible. The cloud's upper portion includes the anvil. Accompanying precipitation is often heavy and the usual occurrence of lightning and thunder with these clouds leads to the popular names of thunderhead or thundercloud. See also Thunderstorm. CUMULUS CLOUD -- A column of rising air that has condensed into a dense, non - fibrous cloud with distinct outlines, appearing much like a rising mound, a dome, or cauliflower. The base of the cloud is relatively flat and dark, while the tower is usually white and sunlit. The cumulus cloud is the first stage of a developing thunderstorm, although most cumulus do not form thunder- storms. DOWNDRAFT -- A column of generally cool air that rapidly sinks to the ground, most often accompanied by precipitation in a shower or thunderstorm. Areas of downdraft usually contain little cloud, and what clouds that may be present are typically dissipating. FLANKING LINE -- A line of cumulus connected to and extending outward from the most active portion of a parent cumulonimbus, usually found on the southwest side of the storm. The cloud line has roughly a stair step appearance with the taller clouds adjacent to the parent cumulonimbus. It is most frequently associated with strong or severe thunderstorms. FLASH FLOODING -- Flooding that develops very quickly on streams and river tributaries usually as a result of thunderstorms. Sometimes the onset of flash flooding comes before the end of heavy rains. There is little time between the detection of flood conditions and the arrival of the flood crest. Swift action is essential to the protection of life and property. FRONT -- A transition zone between two differing air masses. Basic frontal types are (1) COLD FRONT where cooler air advances replacing warmer air; (2) WARM FRONT -- warmer air advances replacing cooler air; (3) STATIONARY FRONT -- warmer air meeting cooler air with neither air mass moving appreciably. Thunderstorms can form in association with any of these fronts. However, fronts are not necessary for thunderstorm development. -2- FUNNEL CLOUD -- A funnel- shaped cloud extending from a towering cumulus or cumulonimbus base. It is associated with a rotating air column that is not in contact with the ground. The cloud is a tornado if a ground -based debris or dust whirl is visible below the funnel aloft. GUST FRONT -- The leading edge of the thunderstorm downdraft air. The gust front is most prominent beneath the rain -free base and on the leading edge of an approaching thunderstorm. It is usually marked by gusty, cool winds, and sometimes blowing dust. The gust front often precedes the thunderstorm precipitation by several minutes. The shelf or roll cloud sometimes accompanies the gust front, especially when the gust front precedes a line of thunderstorms. HAIL -- Precipitation in the form of balls or clumps of ice, produced by thunder- storms. Severe storms with intense updrafts are the most likely large hail producers. HOOK ECHO -- A radar pattern sometimes observed in the southwest quadrant of a tornadic thunderstorm. Appearing like the number six or a fishhook turned in toward the east, the hook echo is precipitation aloft around the periphery of a rotating column of air 2 -10 miles in diameter. The hook echo is often found in a local area favorable for tornado development. However, many tornadoes occur without a hook echo and not all hook echoes produce tornadoes. LIGHTNING -- Any and all of the various forms of visible electrical discharge caused by thunderstorms. Severe thunderstorms usually have very frequent and sometimes nearly continuous lightning. However, some non - severe thunderstorms also contain frequent and vivid electrical displays, while some severe storms are accompanied by little lightning. MAMMA CLOUDS -- Also called mammatus, these clouds appear as hanging, rounded protuberances or pouches on the under surface of a cloud, With thunderstorms, mammatus are seen on the underside of the anvil. These clouds do not produce tornadoes, funnels, hail, or any other type of severe weather, altFough they often accompany severe thunderstorms. • PRECIPITATION SHAFT -- A visible column of rain and /or hail falling from a cloud base. When viewed against a light background, heavy precipitation appears very dark gray, sometimes with a turquoise tinge. This turquoise tinge has been commonly attributed to hail but its actual cause is unknown. RAIN-FREE BASE -- A horizontal, dark cumulonimbus base that has no visible precipitation beneath it. This structure usually marks the location of the thunderstorm updraft. Tornadoes most commonly develop (1) from wall clouds that are attached to the rain -free base, or (2) from the rain -free base itself. This is particularly true when the rain -free base is observed to the south or southwest of the precipitation shaft. RIVER FLOOD -- Occurs on rivers, usually after flash flooding has occurred on streams and tributaries. River floods develop and reach their peak more slowly than flash floods. In many cases, the river flood peak occurs after the rain has ended. -3- ROLL CLOUD -- A relatively rare low- level, horizontal tube - shaped accessory cloud completely detached from the cumulonimbus base. When present, it is located along the gust front and most frequently observed on the leading edge of a line of thunderstorms. The roll cloud will appear to be slowly "rolling" about its horizontal axis. Roll clouds are not and do not produce tornadoes. SCUD CLOUDS -- Low cloud fragments often seen in association with and behind thunderstorm gust fronts. These clouds are ragged and wind torn and are not usually attached to the thunderstorm base. Scud clouds do not produce severe weather. In some cases, when scud clouds are attached to the thunderstorm base they can be mistaken for wall clouds or tornadoes. SEVERE THUNDERSTORM -- A thunderstorm that goes from the mature stage to the severe stage before dissipating. Severe thunderstorms are most efficient "machines" because the updraft remains separated from the downdraft. They also occasionally contain rotation on a broad scale. Because of its structure, the severe storm may last for hours beyond the lifetime of a normal thunder- storm while producing large hail, high winds, torrential rain, and possible tornadoes. Officially, a thunderstorm is classified as severe if 50 knot (58 mph) winds are measured, 3/4 inch or larger hail occurs, or funnel clouds or tornadoes develop. STRAIGHT WINDS -- Winds associated with a thunderstorm, most frequently found with the gust front. These winds originate as downdraft air reaches the ground and rapidly spreads out, becoming strong horizontal flow. Damaging straight winds, although relatively rare themselves, are much more common than are tornadoes. SHELF CLOUD -- A low -level horizontal accessory cloud that frequently appears to be wedge- shaped as it approaches. It is usually attached to the thunder- storm base and forms along the gust front. The leading edge of the shelf is often smooth and at times layered or terraced. The underside is concave upward, turbulent, boiling, or wind torn and often is marked by light and dark areas. It is most often seen along the leading edge of an approaching line of thunder- storms, accompanied by gusty straight winds as it passes overhead and followed by precipitation. Tornadoes rarely occur with the shelf cloud. SQUALL LINE -- Any line or narrow band of active thunderstorms. The term is usually used to describe solid or broken lines of strong or severe thunderstorms. TAIL CLOUD -- A low tail- shaped cloud extending outward from the northern quadrant of a wall cloud. Motions in the tail cloud are toward the wall cloud with rapid updraft at the junction of tail and wall cloud. This horizontal cloud is not a funnel or tornado. THUNDERSTORM -- A local storm (accompanied by lightning and thunder) produced by a cumulonimbus cloud, usually with gusty winds, heavy rain, and sometimes hail. Non - severe thunderstorms rarely have lifetimes over two hours. A typical, non - severe thunderstorm life cycle consists of three stages: (1) CUMULUJ STAGE -- warm, moist air rises (updraft) and condenses into tiny water droplets which make up the visible cloud. (2) MATURE STAGE -- the cloud grows above the freezing level; precipitation forms and becomes heavy enough to fall back to earth. This precipitation generates cool air which also sinks -4- back to earth with the precipitation. (3) DISSIPATION STAGE -- Cool rain and downdraft spread throughout the storm replacing the updraft which is the lifeblood of the thunderstorm. The visible cumulonimbus cloud becomes softer in appearance, less distinctly outlined or "fuzzy" and dissipates, sometimes leaving only the high anvil cloud, as the storm rains itself out. TORNADO -- A violently rotating narrow column of air in contact with the ground and extending from a thunderstorm base. The tornado is most often found in the southwest quadrant of the storm, near the trailing edge of the cumulonimbus cloud. Research observations indicate that tornadoes and funnel clouds are usually pendant from (1) wall clouds or (2) directly from the thunderstorm base, within a few miles to the southwest of the precipitation shaft. The spinning motion of a tornado is most often left to right on the front side and right to left on the backside (counterclockwise). Tornadoes have been called twisters and cyclones, but these words are all synonyms for the most violent storm on earth with estimated wind speeds up to 300 mph. UPDRAFT -- Warm moist air which rises and condenses into a visible cumulus or cumulonimbus cloud. Once the cloud forms; it depends on the updraft for continuance and further development. VIRGA -- Wisps or streaks of rain falling out of a cloud but not reaching the earth's surface. When seen from a distance, these streaks can be mistaken for funnels or tornadoes. WALL CLOUD -- A local and often abrupt lowering of a rain -free cumulonimbus base into a low- hanging accessory cloud, from 1 to 4 miles in diameter. The wall cloud is usually situated in the southwest portion of the storm below an intense updraft, marked by the main cumulonimbus cloud and associated with a very strong or severe thunderstorm. When seen from within several miles, many wall clouds exhibit rapid upward motion and rotation in the same sense as a tornado, except with considerably slower speed. A rotating wall cloud usually develops before tornadoes or funnel clouds by a time which can range from a few minutes up to possibly an hour. Spotters should key on any lowering of the cumulonimbus base as a suspect wall cloud, particularly when it is located southwest of the precipitation shaft. Wall clouds should be reported. Note: Sometimes other low- hanging accessory clouds are mistakenly identified as wall clouds. WARNING -- (issued for tornadoes, severe thunderstorm, flash flood, river flood.) A warning is issued when severe weather has already developed and has been reported by spotters or indicated by radar. Warnings are statements of imminent danger and are issued for relatively small areas near and downstream from the severe storm or flood. WATCH -- (issued for tornado, severe thunderstorm, flash flood.) A watch identifies a relatively large area in which flash floods or severe storms might occur. Watches are quite often issued before any severe weather has developed. Severe thunderstorm and tornado watches usually include an area 140 miles wide by about 200 miles long. The watch is only an indication of where and when the severe weather probabilities are highest, and should not be confused with a warning. -5- These definitions cover much of the material presented in the SKYWARN training session. The different portions of a typical tornadic storm are diagrammed on pages 6 and 7 of this guide. REPORTING CRITERIA ESTIMATING HAIL SIZE 1. Wall Cloud, Funnel or Tornado pea size 1/4 inch 2. Hail 1/4 in. or greater marble 1/2 inch 3. Damaging winds 50 mph or more dime 3/4 inch 4. Flash Flooding quarter 1 inch 5. 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(f) O mac— �--_ Z art • k' �. � .. � : o U tif :M 2 j 0 U • . • 4"""r" 1 i .i.••• ■■••"`" N ‘, :::- w ''.21.0100" \ :.. x 0 - . \ ::: cn • if--0 0 0 •. 9WO 0 0 . 0 0 0 :r. LO vv 2 • � o : . . .,,, . 0 • 7 \SHEI ANVIL EDGE id d i a _ 0 . V • 0,04P DEVELOPING • 'CUMULUS TOWERS i• Light rain SCHEMATIC VIEW OF A SQUALL Moderate rain 1 LINE, LOOKING DOWN MEM Heavy rain and Scale possible email hoil 0 10 20 30 40 50 km t 0 5 10 15 20 25 n mi ATTENDANCE ROSTER TORNADO AND SEVERE WEATHER MEETING April 10, 1990 NAME TELEPHONE REPRESENTING James Q. Joines 589 -2410 Pct. 2 Vol. Fire Dept. Abe Fonseca 776 -3731 Tx. Highway Patrol Mike Mathews 764 -3600 C. S. Police Dept. Bill Williamsen 361 -4478 Constable Pct. 7 Earl Adams 778 -1214 Brazos County REACT Duncan Covington 693 -8000 Rain Gauge Network Alvin R. Phelps 822 -0885 Pct. 4 Vol. Fire Dept. Peggy Crittenden 764 -5402 C.S. Ind. Sch. Dist. John Padgett 823 -8471 TAMU Riversides Campus J. M. Beamer 361 -4100 Brazos Cty. Sheriff's. Steve Beachy 764 -3773 C.S. Emer. Mgmt. Coord. Dean Dyer 776 -5402 Red Cross Robert E. Foust 845 -2345 TAMU Police Dept. Ron Mayworm 846 -0845 Pct. 3 Vol. Fire Dept. Harry Stiteler, Jr. 845 -2132 TAMU Em. Mgt. Coord. Dick Zimmer 845 -6385 RACES Arthur Olden 690 -6819 Tornado Spotters Thomas Goehl 764 -3700 C.S. Fire Dept. William (Bill) Lewis 361 -4450 Braz. Cty. Health Dept. David G. Jefferson 361 -4450 Braz. Cty. Health Dept. Bill Moore 361 -5200 Bryan Ind. Sch. Dist. Henry Colwell 361 -5200 Bryan Ind. Sch. Dist. Anne Beamer 776 -3731 Dept. Pub. Safety Jane Adams 778 -1241 Braz. Cty. REACT Bobby Clay 822 -0061 Bryan Police Dept. Bobby Maddox 361 -3738 Bryan Police Dept. Liz McDonald 779 -4663 GTE Donny Baron 779 -4616 GTE A. H. Winder 822 -2127 Braz. Cty. Engineers Frank Palermo 822 -2127 Braz. Cty. Engineers Naomi Giroux 764 -5276 Humana Hospital Reed Edmundson 690 -0039 Greenleaf Hospital -2- NAME TELEPHONE REPRESENTING JoAnn Jensen 846 -3998 Federal Aviation Adm. Darwin L. Klontz 846 -3998 FAA - C.S. ATCT Jeff Haislet 779 -0911 Braz. Cty. 911 Dist. Geneva Brewer Johnston 845 -5171 TAMU Communications Richard Arnold 845 -4811 Easterwood Airport Larry Jackson 845 -5613 KAMU -FM (TAMU) Charles W. Phelps 822 -0078 Bryan Police Dept. Mary Kaye Moore 361 -3603 City of Bryan Chuck R. Clements 846 -1150 WTAW /KTSR John V. Blackburn 361 -3607 City of Bryan Cathy Hans 690 -0039 HCA Greenleaf Bill Schaer 764 -3712 C.S. Ambulance Garry Lange 764 -3682 C.S. Elec. Dist. Augie Talmisano 764 -3638 C.S. Utility Ops. John Prihoda 845 -5611 KAMU -TV Ernest Clark - 361 -3601 City Mgr. Bryan Will Skopik 361 -3683 Bryan Fire Dept. Sherylon Carroll 846 -1150 WTAW -KTSR Radio A TT L WDAWc TE ROsTE k. N AM E IELEptioNE REV&EENTIN& A,ve ( J 0 ;A/es �t�9- - 1?- 0W /o ?ef iii a56 61(156=G) 4 776, .37 3 i T gil ( PA,---c-r2A__ )Vi 1 114 7/ = ws yew- iy -3 ,e.;) .4 . -,s . fp, ? ;t( t ((i' rvisew 40 9 3(/ 44-78 Co ,ds t %, 77 / 2- ly /1,2 ..-- , ,-z T ,0 /4,.. . . 6 - i2--, ,) . 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