Richmond, VA Hurricanes
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Waste Management Strategy for the British Virgin Islands Ministry of Health & Social Development
FINAL REPORT ON WASTE MANAGEMENT WASTE CHARACTERISATION STRATEGY FOR THE BRITISH J U L Y 2 0 1 9 VIRGIN ISLANDS Ref. 32-BV-2018Waste Management Strategy for the British Virgin Islands Ministry of Health & Social Development TABLE OF CONTENTS LIST OF ACRONYMS..............................................................................2 1 INTRODUCTION.........................................................3 1.1 BACKGROUND OF THE STUDY..........................................................3 1.2 SUBJECT OF THE PRESENT REPORT..................................................3 1.3 OBJECTIVE OF THE WASTE CHARACTERISATION................................3 2 METHODOLOGY.........................................................4 2.1 ORGANISATION AND IMPLEMENTATION OF THE WASTE CHARACTERISATION....................................................................4 2.2 LIMITATIONS AND DIFFICULTIES......................................................6 3 RESULTS...................................................................7 3.1 GRANULOMETRY.............................................................................7 3.2 GRANULOMETRY.............................................................................8 3.2.1 Overall waste composition..................................................................8 3.2.2 Development of waste composition over the years..........................11 3.2.3 Waste composition per fraction........................................................12 3.3 STATISTICAL ANALYSIS.................................................................17 -
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. -
BUYOUTS and BEYOND: Politics, Planning, and the Future of Staten Island's East Shore After Superstorm Sandy
BUYOUTS AND BEYOND: Politics, Planning, and the Future of Staten Island’s East Shore After Superstorm Sandy By Alexander F. Brady B.A. Comparative Literature Princeton University, 2010 SUBMITTED TO THE DEPARTMENT OF URBAN STUDIES AND PLANNING IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER IN CITY PLANNING AT THE MASSACHUSETTS INSTITUTE OF TECHNOLOGY JUNE 2015 ©2015 Alexander F. Brady. All Rights Reserved. The author hereby grants to MIT permission to reproduce and to distribute publicly paper and electronic copies of this thesis document in whole or in part in any medium now known or hereafter created. Signature of Author ____________________________________________________________________________________ Department of Urban Studies and Planning May 18, 2015 Certified by ____________________________________________________________________________________________ Professor Lawrence J. Vale Department of Urban Studies and Planning Thesis Supervisor Accepted by ___________________________________________________________________________________________ Professor Dennis Frenchman Chair, MCP Committee Department of Urban Studies and Planning BUYOUTS AND BEYOND: Politics, Planning, and the Future of Staten Island’s East Shore After Superstorm Sandy By Alexander F. Brady B.A. Comparative Literature Princeton University, 2010 Submitted to the Department of Urban Studies and Planning on May 18th, 2015 in Partial Fulfillment of the Requirements for the Degree of Master in City Planning ABSTRACT In the aftermath of Superstorm Sandy, two separate, federally funded programs began purchasing storm-damaged homes from voluntary sellers in the low-lying, working- class communities of Staten Island’s East Shore. New York State’s, offered in three specific, geographically bounded neighborhoods, requires that the land procured be preserved as open space. The City’s acquires any substantially damaged properties, with the goal of redeveloping them as more resilient housing. -
Hurricane Ernesto (2006): Frontal Influence on Precipitation Distribution
Hurricane Ernesto (2006): Frontal Influence on Precipitation Distribution Jordan Dale and Gary Lackmann North Carolina State University Barrett Smith NOAA/National Weather Service Raleigh, North Carolina Motivation Observational Analysis Simulated Frontal Analysis • The distribution of precipitation associated with landfalling tropical 0600 UTC 1 September 0600 UTC 1 September cyclones remains a critical forecast problem and is dependent on several factors, including: . storm motion . intensity . areal extent . synoptic-scale forcing Surface observations RUC Theta and 2-D Frontogenesis 0.5° Reflectivity Theta and 2-D Frontogenesis 850mb Temperature Advection Simulated Total Reflectivity . topographical characteristics • A warm front is noted by a theta gradient strong frontogenesis along the • The locations of frontogenesis and theta gradients with respect to the TC . mesoscale boundaries center are similar to observations but displaced westward. Enhanced coast east of the TC center. A region of enhanced reflectivity is north of • Of these factors, mesoscale boundaries are a prominent forecasting the warm front near the TC center. reflectivities are present to the north of the frontal boundary in locations challenge due to the small spatial scales and complex origins. where 850mb warm advection is occurring. 1800 UTC 1 September • The purpose of this study is to isolate the physical processes at play 1800 UTC 1 September during the interaction of tropical cyclones (TC) and boundaries, and then investigate the predictability and impact -
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. -
Hurricane and Tropical Storm
State of New Jersey 2014 Hazard Mitigation Plan Section 5. Risk Assessment 5.8 Hurricane and Tropical Storm 2014 Plan Update Changes The 2014 Plan Update includes tropical storms, hurricanes and storm surge in this hazard profile. In the 2011 HMP, storm surge was included in the flood hazard. The hazard profile has been significantly enhanced to include a detailed hazard description, location, extent, previous occurrences, probability of future occurrence, severity, warning time and secondary impacts. New and updated data and figures from ONJSC are incorporated. New and updated figures from other federal and state agencies are incorporated. Potential change in climate and its impacts on the flood hazard are discussed. The vulnerability assessment now directly follows the hazard profile. An exposure analysis of the population, general building stock, State-owned and leased buildings, critical facilities and infrastructure was conducted using best available SLOSH and storm surge data. Environmental impacts is a new subsection. 5.8.1 Profile Hazard Description A tropical cyclone is a rotating, organized system of clouds and thunderstorms that originates over tropical or sub-tropical waters and has a closed low-level circulation. Tropical depressions, tropical storms, and hurricanes are all considered tropical cyclones. These storms rotate counterclockwise in the northern hemisphere around the center and are accompanied by heavy rain and strong winds (National Oceanic and Atmospheric Administration [NOAA] 2013a). Almost all tropical storms and hurricanes in the Atlantic basin (which includes the Gulf of Mexico and Caribbean Sea) form between June 1 and November 30 (hurricane season). August and September are peak months for hurricane development. -
Report of the Governor's Commission to Rebuild Texas
EYE OF THE STORM Report of the Governor’s Commission to Rebuild Texas John Sharp, Commissioner BOARD OF REGENTS Charles W. Schwartz, Chairman Elaine Mendoza, Vice Chairman Phil Adams Robert Albritton Anthony G. Buzbee Morris E. Foster Tim Leach William “Bill” Mahomes Cliff Thomas Ervin Bryant, Student Regent John Sharp, Chancellor NOVEMBER 2018 FOREWORD On September 1 of last year, as Hurricane Harvey began to break up, I traveled from College Station to Austin at the request of Governor Greg Abbott. The Governor asked me to become Commissioner of something he called the Governor’s Commission to Rebuild Texas. The Governor was direct about what he wanted from me and the new commission: “I want you to advocate for our communities, and make sure things get done without delay,” he said. I agreed to undertake this important assignment and set to work immediately. On September 7, the Governor issued a proclamation formally creating the commission, and soon after, the Governor and I began traveling throughout the affected areas seeing for ourselves the incredible destruction the storm inflicted Before the difficulties our communities faced on a swath of Texas larger than New Jersey. because of Harvey fade from memory, it is critical that Since then, my staff and I have worked alongside we examine what happened and how our preparation other state agencies, federal agencies and local for and response to future disasters can be improved. communities across the counties affected by Hurricane In this report, we try to create as clear a picture of Harvey to carry out the difficult process of recovery and Hurricane Harvey as possible. -
Hurricane Irma Storm Review
Hurricane Irma Storm Review November 11, 2018 At Duke Energy Florida, we power more than 4 million lives Service territory includes: . Service to 1.8 million retail customers in 35 counties . 13,000 square miles . More than 5,100 miles of transmission lines and 32,000 miles of distribution lines . Owns and operates nearly 9,500 MWs of generating capacity . 76.2% gas, 21% coal, 3% renewable, 0.2%oil, 2,400 MWs Purchased Power. 2 Storm Preparedness Activities Operational preparation is a year-round activity Coordination with County EOC Officials . Transmission & Distribution Systems Inspected and . Structured Engagement and Information Maintained Sharing Before, During and After Hurricane . Storm Organizations Drilled & Prepared . Coordination with county EOC priorities . Internal and External Resource Needs Secured . Public Communications and Outreach . Response Plan Tested and Continuously Improved Storm Restoration Organization Transmission Hurricane Distribution System Preparedness System Local Governmental Coordination 3 Hurricane Irma – Resources & Logistics Resources . 12,528 Total Resources . 1,553 pre-staged in Perry, Georgia . 91 line and vegetation vendors from 25 states . Duke Energy Carolinas and Midwest crews as well as resources from Texas, New York, Louisiana, Colorado, Illinois, Oklahoma, Minnesota, Maine and Canada . 26 independent basecamps, parking/staging sites Mutual Assistance . Largest mobilization in DEF history . Mutual Assistance Agreements, executed between DEF and other utilities, ensure that resources can be timely dispatched and fairly apportioned. Southeastern Electric Exchange coordinates Mutual Assistance 4 5. Individual homes RESTORATION 3. Critical Infrastructure 2. Substations 1. Transmission Lines 4. High-density neighborhoods 5 Hurricane Irma- Restoration Irma’s track northward up the Florida peninsula Restoration Summary resulted in a broad swath of hurricane and tropical Customers Peak Customers Outage storm force winds. -
Background Hurricane Katrina
PARTPART 33 IMPACTIMPACT OFOF HURRICANESHURRICANES ONON NEWNEW ORLEANSORLEANS ANDAND THETHE GULFGULF COASTCOAST 19001900--19981998 HURRICANEHURRICANE--CAUSEDCAUSED FLOODINGFLOODING OFOF NEWNEW ORLEANSORLEANS •• SinceSince 1559,1559, 172172 hurricaneshurricanes havehave struckstruck southernsouthern LouisianaLouisiana ((ShallatShallat,, 2000).2000). •• OfOf these,these, 3838 havehave causedcaused floodingflooding inin NewNew thethe OrleansOrleans area,area, usuallyusually viavia LakeLake PonchartrainPonchartrain.. •• SomeSome ofof thethe moremore notablenotable eventsevents havehave included:included: SomeSome ofof thethe moremore notablenotable eventsevents havehave included:included: 1812,1812, 1831,1831, 1860,1860, 1915,1915, 1947,1947, 1965,1965, 1969,1969, andand 20052005.. IsaacIsaac MonroeMonroe ClineCline USWS meteorologist Isaac Monroe Cline pioneered the study of tropical cyclones and hurricanes in the early 20th Century, by recording barometric pressures, storm surges, and wind velocities. •• Cline charted barometric gradients (right) and tracked the eyes of hurricanes as they approached landfall. This shows the event of Sept 29, 1915 hitting the New Orleans area. • Storm or tidal surges are caused by lifting of the oceanic surface by abnormal low atmospheric pressure beneath the eye of a hurricane. The faster the winds, the lower the pressure; and the greater the storm surge. At its peak, Hurricane Katrina caused a surge 53 feet high under its eye as it approached the Louisiana coast, triggering a storm surge advisory of 18 to 28 feet in New Orleans (image from USA Today). StormStorm SurgeSurge •• The surge effect is minimal in the open ocean, because the water falls back on itself •• As the storm makes landfall, water is lifted onto the continent, locally elevating the sea level, much like a tsunami, but with much higher winds Images from USA Today •• Cline showed that it was then northeast quadrant of a cyclonic event that produced the greatest storm surge, in accordance with the drop in barometric pressure. -
Hurricane Florence CDBG-DR Action Plan North Carolina Office of Recovery and Resiliency
Hurricane Florence CDBG-DR Action Plan North Carolina Office of Recovery and Resiliency February 7, 2020 Hurricane Florence CDBG-DR Action Plan State of North Carolina For CDBG-DR Funds (Public Law 115-254, Public Law 116-20) Hurricane Florence CDBG-DR Action Plan North Carolina Office of Recovery and Resiliency This page intentionally left blank. Hurricane Florence CDBG-DR Action Plan North Carolina Office of Recovery and Resiliency Revision History Version Date Description 1.0 February 7, 2020 Initial Action Plan i Hurricane Florence CDBG-DR Action Plan North Carolina Office of Recovery and Resiliency This page intentionally left blank. ii Hurricane Florence CDBG-DR Action Plan North Carolina Office of Recovery and Resiliency Table of Contents 1.0 Executive Summary ....................................................................................... 1 2.0 Authority ...................................................................................................... 5 3.0 Recovery Needs Assessment ......................................................................... 7 3.1 Hurricane Florence ............................................................................................... 8 3.2 Summary of Immediate Disaster Impacts ............................................................ 13 3.3 Resilience Solutions and Mitigation Needs .......................................................... 20 3.4 Housing Impact Assessment ................................................................................ 21 3.5 HUD Designated -
Hurricane & Tropical Storm
5.8 HURRICANE & TROPICAL STORM SECTION 5.8 HURRICANE AND TROPICAL STORM 5.8.1 HAZARD DESCRIPTION A tropical cyclone is a rotating, organized system of clouds and thunderstorms that originates over tropical or sub-tropical waters and has a closed low-level circulation. Tropical depressions, tropical storms, and hurricanes are all considered tropical cyclones. These storms rotate counterclockwise in the northern hemisphere around the center and are accompanied by heavy rain and strong winds (NOAA, 2013). Almost all tropical storms and hurricanes in the Atlantic basin (which includes the Gulf of Mexico and Caribbean Sea) form between June 1 and November 30 (hurricane season). August and September are peak months for hurricane development. The average wind speeds for tropical storms and hurricanes are listed below: . A tropical depression has a maximum sustained wind speeds of 38 miles per hour (mph) or less . A tropical storm has maximum sustained wind speeds of 39 to 73 mph . A hurricane has maximum sustained wind speeds of 74 mph or higher. In the western North Pacific, hurricanes are called typhoons; similar storms in the Indian Ocean and South Pacific Ocean are called cyclones. A major hurricane has maximum sustained wind speeds of 111 mph or higher (NOAA, 2013). Over a two-year period, the United States coastline is struck by an average of three hurricanes, one of which is classified as a major hurricane. Hurricanes, tropical storms, and tropical depressions may pose a threat to life and property. These storms bring heavy rain, storm surge and flooding (NOAA, 2013). The cooler waters off the coast of New Jersey can serve to diminish the energy of storms that have traveled up the eastern seaboard.