'Service Assessment': Hurricane Isabel September 18-19, 2003
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Observed Hurricane Wind Speed Asymmetries and Relationships to Motion and Environmental Shear
1290 MONTHLY WEATHER REVIEW VOLUME 142 Observed Hurricane Wind Speed Asymmetries and Relationships to Motion and Environmental Shear ERIC W. UHLHORN NOAA/AOML/Hurricane Research Division, Miami, Florida BRADLEY W. KLOTZ Cooperative Institute for Marine and Atmospheric Studies, Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, Florida TOMISLAVA VUKICEVIC,PAUL D. REASOR, AND ROBERT F. ROGERS NOAA/AOML/Hurricane Research Division, Miami, Florida (Manuscript received 6 June 2013, in final form 19 November 2013) ABSTRACT Wavenumber-1 wind speed asymmetries in 35 hurricanes are quantified in terms of their amplitude and phase, based on aircraft observations from 128 individual flights between 1998 and 2011. The impacts of motion and 850–200-mb environmental vertical shear are examined separately to estimate the resulting asymmetric structures at the sea surface and standard 700-mb reconnaissance flight level. The surface asymmetry amplitude is on average around 50% smaller than found at flight level, and while the asymmetry amplitude grows in proportion to storm translation speed at the flight level, no significant growth at the surface is observed, contrary to conventional assumption. However, a significant upwind storm-motion- relative phase rotation is found at the surface as translation speed increases, while the flight-level phase remains fairly constant. After removing the estimated impact of storm motion on the asymmetry, a significant residual shear direction-relative asymmetry is found, particularly at the surface, and, on average, is located downshear to the left of shear. Furthermore, the shear-relative phase has a significant downwind rotation as shear magnitude increases, such that the maximum rotates from the downshear to left-of-shear azimuthal location. -
Hurricane Turns Aurora and District Into a Lake
FEATURING A SPECIAL GUEST SPEAKER WineWine FROM DineDineBERINGER VINEYARDS & R.S.V.P. & 905-773-9329 as space is limited PRICE $65.00 Aurora’s Community Newspaper PRICE $65.00 PER PERSON + TAX & GRATUITY OCTOBER 28TH 7 pm sharp 49 North Lake Road Oak Ridges Vol. 3 No. 1 Week of October 15, 2002 905-727-3300 Renaming policy sacked by council in a recorded vote The controversial Public on July 11 the committee Facilities Renaming Policy pre- approved the draft policy and it pared by the Leisure Services was presented to council for Advisory Committee was back adoption. before Aurora Council last week A week later, the issue was but this time it was defeated on a deferred to the September 17 4-3 recorded vote. general committee meeting and Two councillors who had indicat- staff were directed to obtain public ed earlier support of the proposal opinion regarding the draft policy. were absent when the vote was Eight replies were received from taken. citizens with the majority opposed The issue was brought about to a renaming policy. some time ago when a request There was a controversial debate was received to change the name at the September 17th general of Willow Creek Park to Elizabeth committee meeting and a motion Hader Park, as a tribute to a by Councillor John West to, in young Aurora girl who lost her life effect, leave things alone was in a horseback riding tragedy. defeated. Her death brought about A follow-up motion by Councillor changes in legislation requiring Evelina MacEachern and second- stricter controls for riding stables ed by Councillor David Griffith (the in hopes that such action would two absent from last week's meet- prevent similar-type accidents. -
1- Tropical Cyclone Report Hurricane Isabel 6-19 September 2003 Jack Beven and Hugh Cobb National Hurricane Center Revised 1 Ju
Tropical Cyclone Report Hurricane Isabel 6-19 September 2003 Jack Beven and Hugh Cobb National Hurricane Center revised 1 July 2004 Updated 9 September 2014 for U.S. damage Hurricane Isabel was a long-lived Cape Verde hurricane that reached Category 5 status on the Saffir-Simpson Hurricane Scale. It made landfall near Drum Inlet on the Outer Banks of North Carolina as a Category 2 hurricane. Isabel is considered to be one of the most significant tropical cyclones to affect portions of northeastern North Carolina and east-central Virginia since Hurricane Hazel in 1954 and the Chesapeake-Potomac Hurricane of 1933. a. Synoptic History Isabel formed from a tropical wave that moved westward from the coast of Africa on 1 September. Over the next several days, the wave moved slowly westward and gradually became better organized. By 0000 UTC 5 September, there was sufficient organized convection for satellite- based Dvorak intensity estimates to begin. Development continued, and it is estimated that a tropical depression formed at 0000 UTC 6 September, with the depression becoming Tropical Storm Isabel six hours later. The “best track” chart of Isabel is given in Fig. 1, with the wind and pressure histories shown in Figs. 2 and 3, respectively. The best track positions and intensities are listed in Table 1. Isabel turned west-northwestward on 7 September and intensified into a hurricane. Strengthening continued for the next two days while Isabel moved between west-northwest and northwest. Isabel turned westward on 10 September and maintained this motion until 13 September on the south side of the Azores-Bermuda High. -
Rouge River Rouge River
Rouge River State of the Watershed Report Surface Water Quantity Goal: Surface waters of a quantity, volume and naturally variable rate of flow to: $ protect aquatic and terrestrial life and ecological functions; $ protect human life and property from risks due to flooding; $ contribute to the protection of Lake Ontario as a domestic drinking water source; $ support sustainable agricultural, industrial, and commercial water supply needs; $ support swimming, fishing and the opportunity to safely consume fish; and $ contribute to the removal of Toronto from the Great Lakes list of Areas of Concern. Surface Water Quantity Key Findings: The Main Rouge subwatershed has been subject to significant urbanization with an approximate total impervious cover of 18% as of 2002. Several studies suggest that the maximum impervious cover that a watershed can withstand before experiencing severe hydrologic changes and consequent geomorphic and ecological impacts is approximately 10%. There has been significantly less urbanization in the Little Rouge subwatershed and impervious surfaces make up only 2% of the subwatershed area. As a result, hydrologic impacts and related effects are much less severe than on the Main Rouge River. Average annual flows in the Main Rouge River show a long-term increasing trend of over 1.3% per year in the past 40 years. This rate of increase is significantly greater than that on the Little Rouge River or nearby rural watersheds and is indicative of the effect of urbanization on the hydrologic cycle. The Rouge River has become flashy and now generates high flows in response to rainfall events that caused almost no response in the river prior to widespread development. -
3131 Lower Don River West Lower Don River West 4.0 DESCRIPTION
Lower Don River West Environmental Study Report Remedial Flood Protection Project 4.0 DESCRIPTION OF LOWER DON 4.1 The Don River Watershed The Don River is one of more than sixty rivers and streams flowing south from the Oak Ridges Moraine. The River is approximately 38 km long and outlets into the Keating Channel, which then conveys the flows into Toronto Harbour and Lake Historic Watershed Ontario. The entire drainage basin of the Don urbanization of the river's headwaters in York River is 360 km2. Figure 4.1 and Figure 4.2, on the Region began in the early 1980s and continues following pages, describe the existing and future today. land use conditions within the Don River Watershed. Hydrologic changes in the watershed began when settlers converted the forests to agricultural fields; For 200 years, the Don Watershed has been many streams were denuded even of bank side subject to intense pressures from human vegetation. Urban development then intensified settlement. These have fragmented the river the problems of warmer water temperatures, valley's natural branching pattern; degraded and erosion, and water pollution. Over the years often destroyed its once rich aquatic and during the three waves of urban expansion, the terrestrial wildlife habitat; and polluted its waters Don River mouth, originally an extensive delta with raw sewage, industrial/agricultural marsh, was filled in and the lower portion of the chemicals, metals and other assorted river was straightened. contaminants. Small Don River tributaries were piped and Land clearing, settlement, and urbanization have buried, wetlands were "reclaimed," and springs proceeded in three waves in the Don River were lost. -
International Agencies O World Meteorological Organization (Https
International Agencies o World Meteorological Organization (https://www.wmo.int/pages/index_en.html) o WMO Regional Climate Centers (http://www.wmo.int/pages/prog/wcp/wcasp/rcc/rcc.php) o World Air Quality Index (http://waqi.info) o International Research Institute for Climate and Society (https://iri.columbia.edu/) o Climate Research Institute (http://www.cru.uea.ac.uk) o Australia Bureau of Meteorology (http://www.bom.gov.au) o Cooperative Institute for Meteorological Studies (http://cimss.ssec.wisc.edu) U.S. Agencies National Centers for Environmental prediction (https://www.ncep.noaa.gov) o Aviation Weather Center (https://aviationweather.gov o Climate Prediction Center (http://www.cpc.noaa.gov) o Environmental Modeling Center (http://www.emc.ncep.noaa.gov) o National Hurricane Center (www.nhc.noaa.gov) o Ocean Prediction Center (http://www.opc.ncep.noaa.gov) o Space Weather Prediction Center (https://www.swpc.noaa.gov) o Storm Prediction Center (www.spc.noaa.gov) o Weather Prediction Center (www.wpc.ncep.noaa.gov) National Oceanic and Atmospheric Administration (https://noaa.gov) National Centers for Environmental Prediction (https://www.ngdc.noaa.gov) Formerly National Geophysical Data Center and National Climate Data Center National Severe Storms Laboratory (http://www.nssl.noaa.gov/) National Snow and Ice Data Center (http://nsidc.org/) National Operational Hydrologic Remote Sensing Center (www.nohrsc.noaa.gov) National Drought Mitigation Center (https://drought.unl.edu/) National Environmental Satellite, Data, & Information Service -
A Rapid Forecasting and Mapping System of Storm Surge and Coastal Flooding
AUGUST 2020 Y A N G E T A L . 1663 A Rapid Forecasting and Mapping System of Storm Surge and Coastal Flooding KUN YANG,VLADIMIR A. PARAMYGIN, AND Y. PETER SHENG Department of Civil and Coastal Engineering, University of Florida, Gainesville, Florida (Manuscript received 16 July 2019, in final form 2 March 2020) ABSTRACT A prototype of an efficient and accurate rapid forecasting and mapping system (RFMS) of storm surge is presented. Given a storm advisory from the National Hurricane Center, the RFMS can generate a coastal inundation map on a high-resolution grid in 1 min (reference system Intel Core i7–3770K). The foundation of the RFMS is a storm surge database consisting of high-resolution simulations of 490 optimal storms generated by a robust storm surge modeling system, Curvilinear-Grid Hydrodynamics in 3D (CH3D-SSMS). The RFMS uses an efficient quick kriging interpolation scheme to interpolate the surge response from the storm surge database, which considers tens of thousands of combinations of five landfall parameters of storms: central pressure deficit, radius to maximum wind, forward speed, heading direction, and landfall location. The RFMS is applied to southwest Florida using data from Hurricane Charley in 2004 and Hurricane Irma in 2017, and to the Florida Panhandle using data from Hurricane Michael in 2018 and validated with observed high water mark data. The RFMS results agree well with observation and direct simulation of the high-resolution CH3D- SSMS. The RFMS can be used for real-time forecasting during a hurricane or ‘‘what-if’’ scenarios for miti- gation planning and preparedness training, or to produce a probabilistic flood map. -
Dodging the 'Perfect Storm'
Dodging the ‘Perfect Storm’ Conservation Ontario’s Business Case for Strategic Reinvestment in Ontario’s Flood Management Programs, Services, and Structures September 2013 Introduction Flooding in Calgary, Alberta and more recently in Toronto, Ontario reminds us just how vulnerable we are when it comes to extreme weather events. The loss of life, devastation, long term social and economic disruption and the staggering cleanup costs in the aftermath of these floods clearly demonstrates how essential it is to have actionable guidelines, policies and programs in place to manage these events. Flooding in downtown Calgary (2013). Source: CTV News Flooding on the Don Valley Parkway, Toronto (2013). Source: CTV News 1 Dodging the ‘Perfect Storm’ – Conservation Ontario’s Business Case for Strategic Reinvestment in Ontario’s Flood Management Programs and Services, and Structures (2013) In Ontario, flooding is the leading cause of public emergency.1 To date, Ontario’s programs to manage floods and regulate floodplains have proven extremely effective and, indeed, the Ontario government has been a leading jurisdiction in Canada for flood planning and management. While much has been accomplished, several factors, if not addressed directly and quickly, will significantly jeopardize the ability of Conservation Authorities and all levels of governments to maintain and improve on this level of management and protection. Flood management is a shared responsibility in Ontario and Conservation Authorities are on the front lines of the Provincial Flood Forecasting and Warning program. In addition, Conservation Authorities bring added protection and benefits through watershed planning, watershed stewardship/natural heritage system management, monitoring and many other programs they deliver. -
Worldwide Marine Radiofacsimile Broadcast Schedules
WORLDWIDE MARINE RADIOFACSIMILE BROADCAST SCHEDULES U.S. DEPARTMENT OF COMMERCE NATIONAL OCEANIC and ATMOSPHERIC ADMINISTRATION NATIONAL WEATHER SERVICE January 14, 2021 INTRODUCTION Ships....The U.S. Voluntary Observing Ship (VOS) program needs your help! If your ship is not participating in this worthwhile international program, we urge you to join. Remember, the meteorological agencies that do the weather forecasting cannot help you without input from you. ONLY YOU KNOW THE WEATHER AT YOUR POSITION!! Please report the weather at 0000, 0600, 1200, and 1800 UTC as explained in the National Weather Service Observing Handbook No. 1 for Marine Surface Weather Observations. Within 300 nm of a named hurricane, typhoon or tropical storm, or within 200 nm of U.S. or Canadian waters, also report the weather at 0300, 0900, 1500, and 2100 UTC. Your participation is greatly appreciated by all mariners. For assistance, contact a Port Meteorological Officer (PMO), who will come aboard your vessel and provide all the information you need to observe, code and transmit weather observations. This publication is made available via the Internet at: https://weather.gov/marine/media/rfax.pdf The following webpage contains information on the dissemination of U.S. National Weather Service marine products including radiofax, such as frequency and scheduling information as well as links to products. A listing of other recommended webpages may be found in the Appendix. https://weather.gov/marine This PDF file contains links to http pages and FTPMAIL commands. The links may not be compatible with all PDF readers and e-mail systems. The Internet is not part of the National Weather Service's operational data stream and should never be relied upon as a means to obtain the latest forecast and warning data. -
NWS Unified Surface Analysis Manual
Unified Surface Analysis Manual Weather Prediction Center Ocean Prediction Center National Hurricane Center Honolulu Forecast Office November 21, 2013 Table of Contents Chapter 1: Surface Analysis – Its History at the Analysis Centers…………….3 Chapter 2: Datasets available for creation of the Unified Analysis………...…..5 Chapter 3: The Unified Surface Analysis and related features.……….……….19 Chapter 4: Creation/Merging of the Unified Surface Analysis………….……..24 Chapter 5: Bibliography………………………………………………….…….30 Appendix A: Unified Graphics Legend showing Ocean Center symbols.….…33 2 Chapter 1: Surface Analysis – Its History at the Analysis Centers 1. INTRODUCTION Since 1942, surface analyses produced by several different offices within the U.S. Weather Bureau (USWB) and the National Oceanic and Atmospheric Administration’s (NOAA’s) National Weather Service (NWS) were generally based on the Norwegian Cyclone Model (Bjerknes 1919) over land, and in recent decades, the Shapiro-Keyser Model over the mid-latitudes of the ocean. The graphic below shows a typical evolution according to both models of cyclone development. Conceptual models of cyclone evolution showing lower-tropospheric (e.g., 850-hPa) geopotential height and fronts (top), and lower-tropospheric potential temperature (bottom). (a) Norwegian cyclone model: (I) incipient frontal cyclone, (II) and (III) narrowing warm sector, (IV) occlusion; (b) Shapiro–Keyser cyclone model: (I) incipient frontal cyclone, (II) frontal fracture, (III) frontal T-bone and bent-back front, (IV) frontal T-bone and warm seclusion. Panel (b) is adapted from Shapiro and Keyser (1990) , their FIG. 10.27 ) to enhance the zonal elongation of the cyclone and fronts and to reflect the continued existence of the frontal T-bone in stage IV. -
A FAILURE of INITIATIVE Final Report of the Select Bipartisan Committee to Investigate the Preparation for and Response to Hurricane Katrina
A FAILURE OF INITIATIVE Final Report of the Select Bipartisan Committee to Investigate the Preparation for and Response to Hurricane Katrina U.S. House of Representatives 4 A FAILURE OF INITIATIVE A FAILURE OF INITIATIVE Final Report of the Select Bipartisan Committee to Investigate the Preparation for and Response to Hurricane Katrina Union Calendar No. 00 109th Congress Report 2nd Session 000-000 A FAILURE OF INITIATIVE Final Report of the Select Bipartisan Committee to Investigate the Preparation for and Response to Hurricane Katrina Report by the Select Bipartisan Committee to Investigate the Preparation for and Response to Hurricane Katrina Available via the World Wide Web: http://www.gpoacess.gov/congress/index.html February 15, 2006. — Committed to the Committee of the Whole House on the State of the Union and ordered to be printed U. S. GOVERNMEN T PRINTING OFFICE Keeping America Informed I www.gpo.gov WASHINGTON 2 0 0 6 23950 PDF 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 COVER PHOTO: FEMA, BACKGROUND PHOTO: NASA SELECT BIPARTISAN COMMITTEE TO INVESTIGATE THE PREPARATION FOR AND RESPONSE TO HURRICANE KATRINA TOM DAVIS, (VA) Chairman HAROLD ROGERS (KY) CHRISTOPHER SHAYS (CT) HENRY BONILLA (TX) STEVE BUYER (IN) SUE MYRICK (NC) MAC THORNBERRY (TX) KAY GRANGER (TX) CHARLES W. “CHIP” PICKERING (MS) BILL SHUSTER (PA) JEFF MILLER (FL) Members who participated at the invitation of the Select Committee CHARLIE MELANCON (LA) GENE TAYLOR (MS) WILLIAM J. -
Richmond, VA Hurricanes
Hurricanes Influencing the Richmond Area Why should residents of the Middle Atlantic states be concerned about hurricanes during the coming hurricane season, which officially begins on June 1 and ends November 30? After all, the big ones don't seem to affect the region anymore. Consider the following: The last Category 2 hurricane to make landfall along the U.S. East Coast, north of Florida, was Isabel in 2003. The last Category 3 was Fran in 1996, and the last Category 4 was Hugo in 1989. Meanwhile, ten Category 2 or stronger storms have made landfall along the Gulf Coast between 2004 and 2008. Hurricane history suggests that the Mid-Atlantic's seeming immunity will change as soon as 2009. Hurricane Alley shifts. Past active hurricane cycles, typically lasting 25 to 30 years, have brought many destructive storms to the region, particularly to shore areas. Never before have so many people and so much property been at risk. Extensive coastal development and a rising sea make for increased vulnerability. A storm like the Great Atlantic Hurricane of 1944, a powerful Category 3, would savage shorelines from North Carolina to New England. History suggests that such an event is due. Hurricane Hazel in 1954 came ashore in North Carolina as a Category 4 to directly slam the Mid-Atlantic region. It swirled hurricane-force winds along an interior track of 700 miles, through the Northeast and into Canada. More than 100 people died. Hazel-type wind events occur about every 50 years. Areas north of Florida are particularly susceptible to wind damage.