Unusual and Noteworthy Meteorological Events at Washington, D.C
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Winter Storms
S. HRG. 109–388 WINTER STORMS HEARING BEFORE THE SUBCOMMITTEE ON DISASTER PREVENTION AND PREDICTION OF THE COMMITTEE ON COMMERCE, SCIENCE, AND TRANSPORTATION UNITED STATES SENATE ONE HUNDRED NINTH CONGRESS SECOND SESSION MARCH 1, 2006 Printed for the use of the Committee on Commerce, Science, and Transportation ( U.S. GOVERNMENT PRINTING OFFICE 27–401 PDF WASHINGTON : 2006 For sale by the Superintendent of Documents, U.S. Government Printing Office Internet: bookstore.gpo.gov Phone: toll free (866) 512–1800; DC area (202) 512–1800 Fax: (202) 512–2250 Mail: Stop SSOP, Washington, DC 20402–0001 VerDate 0ct 09 2002 10:55 May 17, 2006 Jkt 027401 PO 00000 Frm 00001 Fmt 5011 Sfmt 5011 S:\WPSHR\GPO\DOCS\27401.TXT JACKF PsN: JACKF SENATE COMMITTEE ON COMMERCE, SCIENCE, AND TRANSPORTATION ONE HUNDRED NINTH CONGRESS SECOND SESSION TED STEVENS, Alaska, Chairman JOHN MCCAIN, Arizona DANIEL K. INOUYE, Hawaii, Co-Chairman CONRAD BURNS, Montana JOHN D. ROCKEFELLER IV, West Virginia TRENT LOTT, Mississippi JOHN F. KERRY, Massachusetts KAY BAILEY HUTCHISON, Texas BYRON L. DORGAN, North Dakota OLYMPIA J. SNOWE, Maine BARBARA BOXER, California GORDON H. SMITH, Oregon BILL NELSON, Florida JOHN ENSIGN, Nevada MARIA CANTWELL, Washington GEORGE ALLEN, Virginia FRANK R. LAUTENBERG, New Jersey JOHN E. SUNUNU, New Hampshire E. BENJAMIN NELSON, Nebraska JIM DEMINT, South Carolina MARK PRYOR, Arkansas DAVID VITTER, Louisiana LISA J. SUTHERLAND, Republican Staff Director CHRISTINE DRAGER KURTH, Republican Deputy Staff Director KENNETH R. NAHIGIAN, Republican Chief Counsel MARGARET L. CUMMISKY, Democratic Staff Director and Chief Counsel SAMUEL E. WHITEHORN, Democratic Deputy Staff Director and General Counsel LILA HARPER HELMS, Democratic Policy Director SUBCOMMITTEE ON DISASTER PREVENTION AND PREDICTION JIM DEMINT, South Carolina, Chairman TED STEVENS, Alaska E. -
Open Space Plan • Bradford County Subdivision and Land Development Ordinance
Bradford County 2015 Hazard Mitigation Plan Certification of Annual Review Meetings DATE OF PUBLIC OUTREACH YEAR SIGNATURE MEETING ADDRESSED?* 2015 2016 2017 2018 2019 *Confirm yes here annually and describe on record of change page. Page | 1 Bradford County 2015 Hazard Mitigation Plan Record of Changes DESCRIPTION OF CHANGE MADE, CHANGE MADE BY CHANGE MADE BY DATE MITIGATION ACTION COMPLETED, OR (PRINT NAME) (SIGNATURE) PUBLIC OUTREACH PERFORMED Updated profiles for all hazards from the previous mitigation plan and added extreme temperatures, invasive species and radon 09/02/2014 Michael T. Rearick exposure. Updated the mitigation action plan and worked with the municipalities to develop new project opportunities. Completed additional revisions required by 12/17/2014 FEMA. Updated hazard profiles. Added the Michael T. Rearick Levee Failure profile. REMINDER: Please attach all associated meeting agendas, sign-in sheets, handouts, and minutes. Page | 2 Bradford County 2015 Hazard Mitigation Plan Table of Contents Certification of Annual Review Meetings .................................................................................... 1 Record of Changes .................................................................................................................... 2 1. Introduction ......................................................................................................................... 6 1.1 Background ........................................................................................................................................ -
Tuesday, February 2Nd Annual Meeting, 7Pm Mountain Road Library
North Shore on the Magothy www.northshoreaa.com Monday, February 1, 2016 Kassia Gautreau by Sarah Ann Parsons Our final Winner in the Barnacle Header contest is the adorable Kassia Gautreau, the only girl who submitted a drawing for the contest. She is an 8 year old home schooled 2nd grader, having skipped kindergarten, who seems interested in everything. Kassia’s family lived in North Shore for a while but moved to Dallas when she was 2 where they lived for three years. They are now back here for good and although Kassia still misses Dallas and her activities there, she is adjusting well here and enjoying the Tuesday, February community. She likes living across from the 2nd Annual Meeting, 7pm Mountain Road Library February 2016 Issue !1 North Shore on the Magothy www.northshoreaa.com Monday, February 1, 2016 playground and enjoys the beach and the With forecasters calling for a maximum, community parties and get togethers. though unlikely, deluge of up to 27 inches, it might be. She takes ballet, tap and jazz at the Severna Park Dance Academy. This December The county would have to receive more than Kassia danced in “The Nutcracker” with the 26.3 inches to set a new two-day mark. Annapolis Children’s Theater in the part of Mother Ginger’s child and loved it. She That record was set Jan. 27-28, 1922, began dancing when she was in Dallas at during what became known as the the age of two and a half and continues to "Knickerbocker Storm" — named because love it. -
Storm Naming: the First Season of Naming by the South-West Group: Spain-Portugal-France
Storm naming: the First Season of Naming by the South-west Group: Spain-Portugal-France Paula Leitao (IPMA- Instituto Português do Mar e da Atmosfera), Bernard Roulet (Meteo France), Jaime Rey (AEMET) Introduction gust associated with the passage of a storm or low pressure (regional winds such as the Mistral are not Following the success of storm naming by MetEireann taken into account). and the Met Office in 2016-2017 (cf WGCEF Task Team • Area: Atlantic Ocean and western on Storm Naming in Europe ; Authors Cusack, Mediterranean Sea. Paterson, Lang, Csekits, WGCEF newsletter N°22), • The NMS who first issues an orange/red warn- three other countries in the south-western part of ing (or Vigilance) names the storm and informs the Europe - Spain, Portugal and France - decided to join three others. the process of storm naming, following recommenda- • A named Storm keeps the same name its whole tions of the Task Team. life. System specifications were discussed by partners The coordination with the North-west Group is crucial during the year 2017 via mail exchanges, then web- to ensure that the same storm gets a single name. If a conferences during Autumn 2017 allowed the Group storm is named by one group and moves to the other to finalise the process of storm naming for the south- group, it keeps the same name. In the rare cases west. The month of November was then used as a where a barotropic storm is a post-tropical storm, it blank test, before the system entered its operational keeps the name given by NHC Miami preceded by ‘Ex’. -
Ref. Accweather Weather History)
NOVEMBER WEATHER HISTORY FOR THE 1ST - 30TH AccuWeather Site Address- http://forums.accuweather.com/index.php?showtopic=7074 West Henrico Co. - Glen Allen VA. Site Address- (Ref. AccWeather Weather History) -------------------------------------------------------------------------------------------------------- -------------------------------------------------------------------------------------------------------- AccuWeather.com Forums _ Your Weather Stories / Historical Storms _ Today in Weather History Posted by: BriSr Nov 1 2008, 02:21 PM November 1 MN History 1991 Classes were canceled across the state due to the Halloween Blizzard. Three foot drifts across I-94 from the Twin Cities to St. Cloud. 2000 A brief tornado touched down 2 miles east and southeast of Prinsburg in Kandiyohi county. U.S. History # 1861 - A hurricane near Cape Hatteras, NC, battered a Union fleet of ships attacking Carolina ports, and produced high tides and high winds in New York State and New England. (David Ludlum) # 1966 - Santa Anna winds fanned fires, and brought record November heat to parts of coastal California. November records included 86 degrees at San Francisco, 97 degrees at San Diego, and 101 degrees at the International airport in Los Angeles. Fires claimed the lives of at least sixteen firefighters. (The Weather Channel) # 1968 - A tornado touched down west of Winslow, AZ, but did little damage in an uninhabited area. (The Weather Channel) # 1987 - Early morning thunderstorms in central Arizona produced hail an inch in diameter at Williams and Gila Bend, and drenched Payson with 1.86 inches of rain. Hannagan Meadows AZ, meanwhile, was blanketed with three inches of snow. Unseasonably warm weather prevailed across the Ohio Valley. Afternoon highs of 76 degrees at Beckley WV, 77 degrees at Bluefield WV, and 83 degrees at Lexington KY were records for the month of November. -
ANNUAL SUMMARY Atlantic Hurricane Season of 2005
MARCH 2008 ANNUAL SUMMARY 1109 ANNUAL SUMMARY Atlantic Hurricane Season of 2005 JOHN L. BEVEN II, LIXION A. AVILA,ERIC S. BLAKE,DANIEL P. BROWN,JAMES L. FRANKLIN, RICHARD D. KNABB,RICHARD J. PASCH,JAMIE R. RHOME, AND STACY R. STEWART Tropical Prediction Center, NOAA/NWS/National Hurricane Center, Miami, Florida (Manuscript received 2 November 2006, in final form 30 April 2007) ABSTRACT The 2005 Atlantic hurricane season was the most active of record. Twenty-eight storms occurred, includ- ing 27 tropical storms and one subtropical storm. Fifteen of the storms became hurricanes, and seven of these became major hurricanes. Additionally, there were two tropical depressions and one subtropical depression. Numerous records for single-season activity were set, including most storms, most hurricanes, and highest accumulated cyclone energy index. Five hurricanes and two tropical storms made landfall in the United States, including four major hurricanes. Eight other cyclones made landfall elsewhere in the basin, and five systems that did not make landfall nonetheless impacted land areas. The 2005 storms directly caused nearly 1700 deaths. This includes approximately 1500 in the United States from Hurricane Katrina— the deadliest U.S. hurricane since 1928. The storms also caused well over $100 billion in damages in the United States alone, making 2005 the costliest hurricane season of record. 1. Introduction intervals for all tropical and subtropical cyclones with intensities of 34 kt or greater; Bell et al. 2000), the 2005 By almost all standards of measure, the 2005 Atlantic season had a record value of about 256% of the long- hurricane season was the most active of record. -
5.4.1 Severe Storms
SECTION 5.4.1: RISK ASSESSMENT – SEVERE STORM 5.4.1 SEVERE STORMS This section provides a profile and vulnerability assessment for the severe storm hazards. HAZARD PROFILE Hazard profile information is provided in this section, including information on description, extent, location, previous occurrences and losses and the probability of future occurrences within Delaware County. Description For the purpose of this HMP and as deemed appropriated by Delaware County, the severe storm hazard includes hailstorms, windstorms, lightning, thunderstorms, tornadoes, and tropical cyclones (e.g. hurricanes, tropical storms, and tropical depressions), which are defined below. Since most northeasters, (or Nor’Easters) a type of an extra-tropical cyclone, generally take place during the winter weather months, Nor’Easters have been grouped as a type of severe winter weather storm, further discussed in Section 5.4.2 (Severe Winter Storm). Hailstorm: According to the National Weather Service (NWS), hail is defined as a showery precipitation in the form of irregular pellets or balls of ice more than five millimeters in diameter, falling from a cumulonimbus cloud (NWS, 2009). Early in the developmental stages of a hailstorm, ice crystals form within a low-pressure front due to the rapid rising of warm air into the upper atmosphere and the subsequent cooling of the air mass. Frozen droplets gradually accumulate on the ice crystals until, having developed sufficient weight; they fall as precipitation, in the form of balls or irregularly shaped masses of ice. The size of hailstones is a direct function of the size and severity of the storm. High velocity updraft winds are required to keep hail in suspension in thunderclouds. -
The European Forecaster September 2018 (Full Version Pdf)
The European Forecaster Newsletter of the WGCEF N° 23 September 2018 C ontents 3 Introduction Minutes of the 23rd Annual Meeting of the Working Group on Co-operation 4 Between European Forecasters (WGCEF) Sting Jets and other processes leading to high wind gusts: 10 wind-storms “Zeus” and “Joachim” compared 16 Forecasting Freezing Rain in the UK – March 1st and 2nd 2018 24 The Extreme Wildfire, 17-19 July 2017 in Split 30 Changing the Way we Warn for Weather Storm naming: the First Season of Naming by the South-west Group: 33 Spain-Portugal-France 38 Can we forecast the sudden dust storms impacting Israel's southernmost city? 45 The 31st Nordic Meteorological Meeting 46 Representatives of the WGCEF Cover: Ana was the first storm named by the Southwest Group (Spain, Portugal, France) during winter 2017-2018. It affected three countries with great impacts. Printed by Meteo France Editors Stephanie Jameson and Will Lang, Met Office Layout Kirsi Hindstrom- Basic Weather Services Published by Météo-France Crédit Météo-France COM/CGN/PPN - Trappes I ntroduction Dear Readers and Colleagues, It’s a great pleasure to introduce the 23rd edition of our newsletter ‘The European Forecaster’. The publica- tion is only possible due to the great work and generosity of Meteo-France, thus we want to express our warmest gratitude to Mr. Bernard Roulet and his colleagues. We kindly thank all the authors for submitting articles, particularly as they all work in operational forecasting roles and thus have only limited time for writing an article. Many thanks go to Mrs. -
Numerical Simulations of Three Nor'easters
Answers Research Journal 5 (2012):39–58. www.answersingenesis.org/arj/v5/numerical-simulations-noreasters-atlantic.pdf Numerical Simulations of Three Nor’easters with a Warm Atlantic Ocean Larry Vardiman, Institute for Creation Research, 1806 Royal Lane, Dallas, TX 75229 Wesley Brewer, Fluid Physics International, 403-B Santa Anita Drive, Starkville, MS 39759 Abstract Analyses and numerical simulations were conducted on three recent nor’easters which formed on the East Coast of the United States to explore the effects of warmer-than-normal sea-surface temperatures on their wind and precipitation fields. The purpose of the study was to determine how warmer sea-surface temperatures in the Atlantic Ocean following the Genesis Flood would have enhanced nor’easters. Wind and precipitation fields for the actual storms were compared with simulated storms using the NCAR WRF model to insure that the model was accurately replicating the storms. The sea-surface was then increased by about 10°C (18°F) and the models rerun for the three storms. The wind fields and precipitation patterns were compared to the simulated actual storms to find how much the storms had been enhanced and the precipitation footprint changed. The WRF model accurately replicated the actual storms and the warmer sea-surface temperatures dramatically increased the wind speeds and precipitation. The enhanced storms moved more quickly off the Eastern seaboard than the actual storms and formed a larger and heavier snow shield over the northeastern United States and southeastern Canada. The additional accumulation of snow from the larger snow shields likely contributed to the Laurentide Ice Sheet following the Genesis Flood. -
Severe Storm
Section 5.4.5: Risk Assessment – Severe Storm 5.4.5 Severe Storm The following section provides the hazard profile (hazard description, location, extent, previous occurrences and losses, probability of future occurrences, and impact of climate change) and vulnerability assessment for the severe weather hazard in Montgomery County. 5.4.5.1 Profile Hazard Description For the purpose of this HMP and as deemed appropriated by Montgomery County, the severe storm hazard includes hailstorms, windstorms, lightning, thunderstorms, tornadoes, and tropical cyclones [which include tropical depressions, tropical storms, and hurricanes], which are defined below. Since most northeasters, (or Nor’Easters) a type of an extra-tropical cyclone, generally take place during the winter weather months, Nor’Easters have been grouped as a type of severe winter weather storm, further discussed in Section 5.4.6 (Severe Winter Storms). Hailstorm Hail forms inside a thunderstorm where there are strong updrafts of warm air and downdrafts of cold water. If a water droplet is picked up by the updrafts, it can be carried well above the freezing level. Water droplets freeze when temperatures reach 32°F or colder. As the frozen droplet begins to fall, it may thaw as it moves into warmer air toward the bottom of the thunderstorm. However, the droplet may be picked up again by another updraft and carried back into the cold air and re-freeze. With each trip above and below the freezing level, the frozen droplet adds another layer of ice. The frozen droplet, with many layers of ice, falls to the ground as hail. Most hail is small and typically less than two inches in diameter (NWS 2010). -
Center COMAR 13A.16.10 Safety .01 Emergency Safety Requirements. A
Center COMAR 13A.16.10 Safety .01 Emergency Safety Requirements. A. Emergency and Disaster Plan. (1) At least one center employee shall: (a) Complete emergency preparedness training that is approved by the office; and (b) As part of the approved emergency preparedness training, prepare a written emergency and disaster plan for the center. (2) The operator shall maintain the emergency and disaster plan prepared in accordance with § A(1)(b) of this regulation. (3) The emergency and disaster plan shall: (a) Establish procedures for: (i) Evacuating the center, including an evacuation route; (ii) Relocating staff and children to a designated safe site; (iii) Sheltering in place in the event that evacuation is not feasible; (iv) Notifying parents of children in care; and (v) Addressing the individual needs of children, including children with special needs; (b) Contain: (i) The name of, and contact information for the local emergency operations center; (ii) Assignment of staff responsibilities during an emergency or disaster; (iii) A list of local emergency services numbers; and (iv) The radio station call sign and frequency for the local Emergency Alert System; (c) Be practiced by staff and children at least: (i) Once per month for fire evacuation; and (ii) Twice per year for other emergency and disaster situations; and (d) Be updated at least annually. (4) A copy of the emergency escape route floor plan shall be posted in each area and room in the center. (5) Each employee shall be oriented to the contents of the written emergency and disaster plan required at §A(2) of this regulation. -
Application and Verification of ECMWF Products 2018
UK UK Application and verification of ECMWF products 2018 Met Office. Contributing authors: Dan Suri, Marion Mittermaier, Rob Neal, Ric Crocker, Helen Titley and Becky Stretton. 1. Summary of major highlights ECMWF output is widely used by the Met Office at many timescales, especially the week 2 period where the Met Office is particularly dependant on ECMWF output. The heaviest users of ECMWF output are the Chief and Deputy Chief Meteorologists, who provide forecast guidance across the organisation for areas around the world and hydrometeorologists at the Flood Forecasting Centre. ECMWF output also forms part of 'BestData', a multi-model blend producing site-specific forecasts available, for example, on the Met Office public website. Meanwhile, the Met Office have been actively engaged in producing some novel and innovative tools to help operational meteorologists visualize ensemble output, creating and verifying regional weather regime forecasts via a tool known internally as the Decider system and developing a global hazard map, which includes a focus on tropical cyclones. 2. Use and application of products 2.1 Post-processing of ECMWF model output 2.1.1 Statistical adaptation Nothing to report. 2.1.2 Physical adaptation Nothing to report. 2.1.3 Derived fields The end of February and first days of March 2018 saw the most severe outbreak of cold winter weather in the UK for several years, as well as over much of western Europe, compounded by Storm Emma which came from the south and generated exceptional blizzards and freezing rain in the south of the country. The cold outbreak had been well predicted in advance, firstly from long-range predictions of a Sudden Stratospheric Warming increasing the risk of blocking, and then two weeks ahead from the Decider system.