The Impact of Hurricanes on the Weather of Western Europe
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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 -
An Informed System Development Approach to Tropical Cyclone Track and Intensity Forecasting
Linköping Studies in Science and Technology Dissertations. No. 1734 An Informed System Development Approach to Tropical Cyclone Track and Intensity Forecasting by Chandan Roy Department of Computer and Information Science Linköping University SE-581 83 Linköping, Sweden Linköping 2016 Cover image: Hurricane Isabel (2003), NASA, image in public domain. Copyright © 2016 Chandan Roy ISBN: 978-91-7685-854-7 ISSN 0345-7524 Printed by LiU Tryck, Linköping 2015 URL: http://urn.kb.se/resolve?urn=urn:nbn:se:liu:diva-123198 ii Abstract Introduction: Tropical Cyclones (TCs) inflict considerable damage to life and property every year. A major problem is that residents often hesitate to follow evacuation orders when the early warning messages are perceived as inaccurate or uninformative. The root problem is that providing accurate early forecasts can be difficult, especially in countries with less economic and technical means. Aim: The aim of the thesis is to investigate how cyclone early warning systems can be technically improved. This means, first, identifying problems associated with the current cyclone early warning systems, and second, investigating if biologically based Artificial Neural Networks (ANNs) are feasible to solve some of the identified problems. Method: First, for evaluating the efficiency of cyclone early warning systems, Bangladesh was selected as study area, where a questionnaire survey and an in-depth interview were administered. Second, a review of currently operational TC track forecasting techniques was conducted to gain a better understanding of various techniques’ prediction performance, data requirements, and computational resource requirements. Third, a technique using biologically based ANNs was developed to produce TC track and intensity forecasts. -
Portugal – an Atlantic Extreme Weather Lab
Portugal – an Atlantic extreme weather lab Nuno Moreira ([email protected]) 6th HIGH-LEVEL INDUSTRY-SCIENCE-GOVERNMENT DIALOGUE ON ATLANTIC INTERACTIONS ALL-ATLANTIC SUMMIT ON INNOVATION FOR SUSTAINABLE MARINE DEVELOPMENT AND THE BLUE ECONOMY: FOSTERING ECONOMIC RECOVERY IN A POST-PANDEMIC WORLD 7th October 2020 Portugal in the track of extreme extra-tropical storms Spatial distribution of positions where rapid cyclogenesis reach their minimum central pressure ECMWF ERA 40 (1958-2000) Events per DJFM season: Source: Trigo, I., 2006: Climatology and interannual variability of storm-tracks in the Euro-Atlantic sector: a comparison between ERA-40 and NCEP/NCAR reanalyses. Climate Dynamics volume 26, pages127–143. Portugal in the track of extreme extra-tropical storms Spatial distribution of positions where rapid cyclogenesis reach their minimum central pressure Azores and mainland Portugal On average: 1 rapid cyclogenesis every 1 or 2 wet seasons ECMWF ERA 40 (1958-2000) Events per DJFM season: Source: Trigo, I., 2006: Climatology and interannual variability of storm-tracks in the Euro-Atlantic sector: a comparison between ERA-40 and NCEP/NCAR reanalyses. Climate Dynamics volume 26, pages127–143. … affected by sting jets of extra-tropical storms… Example of a rapid cyclogenesis with a sting jet over mainland 00:00 UTC, 23 Dec 2009 Source: Pinto, P. and Belo-Pereira, M., 2020: Damaging Convective and Non-Convective Winds in Southwestern Iberia during Windstorm Xola. Atmosphere, 11(7), 692. … affected by sting jets of extra-tropical storms… Example of a rapid cyclogenesis with a sting jet over mainland Maximum wind gusts: Official station 140 km/h Private station 00:00 UTC, 23 Dec 2009 203 km/h (in the most affected area) Source: Pinto, P. -
17C.7 Atlantic Intense Hurricanes, 1995-2003 – Characteristics Based on Best Track, Aircraft, and Ir Images
17C.7 ATLANTIC INTENSE HURRICANES, 1995-2003 – CHARACTERISTICS BASED ON BEST TRACK, AIRCRAFT, AND IR IMAGES Raymond Zehr* NOAA/NESDIS, Fort Collins, CO 1. INTRODUCTION 2. INTENSITY During the nine-year period 1995-2003, there Hurricane intensity is expressed as the have been 32 intense hurricanes in the Atlantic basin. associated maximum surface wind speed or as the Intense hurricanes are those that attain Saffir-Simpson minimum sea level pressure, which is inversely related Category 3 or higher (i.e. >100 kt wind maximum). A to the wind speed. The lowest minimum sea level distinct upturn in the frequency of intense hurricanes pressure (MSLP) is given in Table 1 along with the has occurred since 1995., with an annual average of 3.6 highest maximum surface wind speed (Vmax) in both intense hurricanes, compared with the long-term (1950- knots and standard units of m/s. It should be noted that 2000) average of 2.3. This change has been Best Track files give intensity measurements at 6-hour documented and discussed by Goldenberg, et al, intervals, which may not capture the maximum intensity. (2001). However, Tropical Prediction Center archives also Using “Best Track” data (Jarvinen and include an estimate of maximum intensity and its time of Neumann, 1979), ordered lists of various parameters occurrence. Hurricane Mitch (1998) was clearly the associated with each of the 32 intense hurricanes have most intense Atlantic hurricane since 1995 with 905 hPa been compiled. For example, the lowest minimum sea- and 155 kt, while the more typical Atlantic intense level pressure (MSLP) with each hurricane ranges from hurricane has MSLP and Vmax of about 940 hPa and 905 hPa with Mitch (1998) to 968 hPa with Erin (2001). -
Variations Aperiodic Extreme Sea Level in Cuba Under the Influence
Extreme non-regular sea level variations in Cuba under the influence of intense tropical cyclones. Item Type Journal Contribution Authors Hernández González, M. Citation Serie Oceanológica, (8). p. 13-24 Publisher Instituto de Oceanología Download date 02/10/2021 16:50:34 Link to Item http://hdl.handle.net/1834/4053 Serie Oceanológica. No. 8, 2011 ISSN 2072-800x Extreme non-regular sea level variations in Cuba under the influence of intense tropical cyclones. Variaciones aperiódicas extremas del nivel del mar en Cuba bajo la influencia de intensos ciclones tropicales. Marcelino Hernández González* *Institute of Oceanology. Ave. 1ra. No.18406 entre 184 y 186. Flores, Playa, Havana, Cuba. [email protected] ACKNOWLEDGEMENTS This work was sponsored by the scientific – technical service "Real Time Measurement and Transmission of Information. Development of Operational Oceanographic Products", developed at the Institute of Oceanology. The author wishes to thank Mrs. Martha M. Rivero Fernandez, from the Marine Information Service of the Institute of Oceanology, for her support in the translation of this article. Abstract This paper aimed at analyzing non-regular sea level variations of meteorological origin under the influence of six major tropical cyclones that affected Cuba, from sea level hourly height series in twelve coastal localities. As a result, it was obtained a characterization of the magnitude and timing of extreme sea level variations under the influence of intense tropical cyclones. Resumen El presente trabajo tuvo como objetivo analizar las variaciones aperiódicas del nivel del mar de origen meteorológico bajo la influencia de seis de los principales ciclones tropicales que han afectado a Cuba, a partir de series de alturas horarias del nivel del mar de doce localidades costeras. -
LBJ Off on Peace Mission; Promises No 'Magic Wand'
Average Daily Net Press Run The Weather For the Week Ended October IK, 1966 Fair, much cooler Umlgntt low 35^0; aunny and a little milder tomorrow, high aow 4^ 1 4 ,9 3 3 Manche»ter~—A City of VMage-Charm (OlMMlltod Advertlalnc on Page U); PRICE SEVEN C E N H VOL. LXXXVIi NO. 14 (TWENTY-FOUR PAGES—TWO SECTIONS) MANCHESTER, CONN., MONDAY, OCTOBER l7 , 1966 i * <' •'fy ' ^ f * r JW. h r ; LBJ Off on Peace Mission; ( ' ■ y - ■ Promises No ‘Magic Wand’ * ( • y ' -' '* « ' ,% i, r -i <■ Honolulu First ’I K I- ■- I ■ -> ‘ . On 25,000-Mile Trip KB. t ■take A tha n it WASHINGTON (AP)—President Johnson departed Oakta. i Rick* on a momentous, 25,000-mile mission to the Far East '« ? , today with a vow to “do my best to advance the cause 'I L of peace and of human progress.” > I- Johnson tempered this pledge -------------------------- — ------- over M with word that “ I know that I corps along the way. A wife or can wave no wand” or offer any g<,t h presidential kiss on a date 1: ' promises to work magic on his u,e ©heek. i S i W i SiMW aerial expedition to at least six on the observation deck far Asian and Pacific nations. above the field, spectators held SittlUL «« he aad Yet, he said, he was undertak- aloft unanimously friendly post i j : « ing “a hopeful mission.” ©i-s bearing such inscriptions as a t aad 1 It was 9:26 a.m. when John- “ All 4 U,” “ U.S.A. -
Documentary Sources to Investigate Multidecadal Variability of Droughts
ISSN 0211-6820 Cuadernos de Investigación Geográfica 2016 Nº 42 (1) pp. 13-27 EISSN 1697-9540 DOI: 10.18172/cig.2936 © Universidad de La Rioja DOCUMENTARY SOURCES TO INVESTIGATE MULTIDECADAL VARIABILITY OF DROUGHTS F. DOMÍNGUEZ-CASTRO1, 2*, R. GARCÍA-HERRERA3, 4 1Departamento de Ingeniería Civil y Ambiental, Escuela Politécnica Nacional, Ecuador. 2Instituto Nacional de Meteorología e Hidrología, Ecuador. 3Dpto. Física de la Tierra II, Universidad Complutense de Madrid, Spain. 4IGEO, Instituto de Geociencias (CSIC, UCM), Spain. ABSTRACT. Droughts are probably the natural hazard with the highest socioeconomic impact. Simultaneously, they are a very complex phenomenon; they are triggered by a diversity of physical factors and occur at a variety of time scales. Consequently, the instrumental record currently available is too short and the characterization of its multidecadal variability requires the use of natural proxies (tree rings, sedimentary records) or documentary sources. In this paper we analyse three documentary sources with potential to analyse the long-term variability of droughts: chapter acts, logbooks and chronicles. The chapter acts recorded discussions and decisions made during the assemblies of the local authorities and provide continuous and direct evidence on drought impacts. They are especially useful to study droughts between the 15th and the 19th centuries in Europe and the 17th to 18th in the former colonies. Logbooks recorded the meteorological conditions and the incidents occurred during navigation. They provide indirect information through the circulation indices that can be very helpful to understand the mechanisms and teleconnections associated to droughts. Finally, the chronicles are historiographical documents describing political and social events. They are secondary sources and the references to climatic events are discontinuous, thus their analysis must be extremely careful, but they are especially useful to study specific drought events especially prior to 15th century when no other sources are available. -
Verification of National Hurricane Center Forecasts of Extratropical Transition
10C.2 Verification of National Hurricane Center Forecasts of Extratropical Transition John L. Beven II NOAA/NWS/NCEP/National Hurricane Center I. Introduction become TCs in a process known as tropical transition (Davis and Bosart 2004). More A great variety of cyclonic circulations commonly, TCs leaving the tropical environment exist in the atmosphere, each with its characteristic interact with baroclinic systems in the westerlies. structure and driving energy (Beven 1997, Figure This causes the TCs to become frontal or 1). Of particular interest is the tropical cyclone extratropical cyclones with the driving energy (TC), which has a warm-core non-frontal thermal derived from air mass contrast and the strongest structure generated by diabatic heat release from winds typically more than 100 km from the center, convective activity near the center. The strongest accompanied by significantly changed winds and heaviest rains in a tropical cyclone are precipitation patterns. This process is known as typically within 100 km of the center with extratropical transition (ET). maximum sustained winds sometimes as high as 90 ms-1. There are several studies of ET which highlight the many ways a TC can interact with a baroclinic environment and the variety of resulting structures. These include the Thorncroft and Jones (2000) study of Hurricane Iris which became a powerful baroclinic cyclone with a warm-core structure, the Abraham et al. (2004) study of Hurricane Michael, and the Beven (2002) study of interrupted and failed transitions. These studies show the complexity of the process, which can pose a significant challenge to TC forecasters trying to predict ET. -
Ex-Hurricane Ophelia 16 October 2017
Ex-Hurricane Ophelia 16 October 2017 On 16 October 2017 ex-hurricane Ophelia brought very strong winds to western parts of the UK and Ireland. This date fell on the exact 30th anniversary of the Great Storm of 16 October 1987. Ex-hurricane Ophelia (named by the US National Hurricane Center) was the second storm of the 2017-2018 winter season, following Storm Aileen on 12 to 13 September. The strongest winds were around Irish Sea coasts, particularly west Wales, with gusts of 60 to 70 Kt or higher in exposed coastal locations. Impacts The most severe impacts were across the Republic of Ireland, where three people died from falling trees (still mostly in full leaf at this time of year). There was also significant disruption across western parts of the UK, with power cuts affecting thousands of homes and businesses in Wales and Northern Ireland, and damage reported to a stadium roof in Barrow, Cumbria. Flights from Manchester and Edinburgh to the Republic of Ireland and Northern Ireland were cancelled, and in Wales some roads and railway lines were closed. Ferry services between Wales and Ireland were also disrupted. Storm Ophelia brought heavy rain and very mild temperatures caused by a southerly airflow drawing air from the Iberian Peninsula. Weather data Ex-hurricane Ophelia moved on a northerly track to the west of Spain and then north along the west coast of Ireland, before sweeping north-eastwards across Scotland. The sequence of analysis charts from 12 UTC 15 to 12 UTC 17 October shows Ophelia approaching and tracking across Ireland and Scotland. -
The Operational Challenges of Forecasting TC Intensity Change in the Presence of Dry Air and Strong Vertical Shear
The Operational Challenges of Forecasting TC Intensity Change in the Presence of Dry Air and Strong Vertical Shear Jamie R. Rhome,* and Richard D. Knabb NOAA/NWS/NCEP/Tropical Prediction Center/National Hurricane Center, Miami, FL 1. INTRODUCTION to an incomplete specification of the initial moisture conditions, dynamical model forecasts of middle- to Tropical cyclone (TC) intensity changes involve upper-tropospheric humidity often have large errors. complex interactions between many environmental Beyond the problems with observing and forecasting factors, including vertical wind shear and the humidity, TC intensity forecasts become particularly thermodynamic properties of the ambient atmosphere challenging when dry air is accompanied by moderate to and ocean. While the effects of each factor are not strong vertical shear. completely understood, even less is known about the Much of the current understanding on the response effects of these factors working in tandem. Emanuel et of a TC to vertical shear comes from idealized studies. It al. (2004) proposed that “storm intensity in a sheared has been shown that strong vertical shear typically results environment is sensitive to the ambient humidity” and in the convective pattern of the TC becoming cautioned “against considering the various environmental increasingly asymmetric followed by a downshear tilt of influences on storm intensity as operating independently the vortex (Frank and Ritchie 2001, Bender 1997). To from each other.” Along these lines, Dunion and Velden keep the tilted TC vortex quasi-balanced, the (2004) have examined the combined effects of vertical diabatically-driven secondary circulation aligns itself to shear and dry air on TCs during interactions with the produce an asymmetry in vertical motion that favors Saharan Air Layer (SAL). -
UB Powerpoint Template
converge.colorado.edu CONVERGE ethical, coordinated, and scientifically rigorous social science, engineering, and interdisciplinary extreme events research Lori Peek Principal Investigator, CONVERGE, SSEER, and ISEEER Director, Natural Hazards Center Professor, Department of Sociology University of Colorado Boulder Session 2: Collecting, Managing, and Archiving Social and Behavioral Science Data Describe opportunities for identifying and coordinating social science researchers so that we can best share information and publish our data as well as data collection protocols using DOIs, repositories, etc. Discuss some of the overarching challenges and concerns with sharing social science data, such as privacy, data management plans and related IRB policies, duplication vs. replication, etc. converge.colorado.edu 4 Things converge.colorado.edu 1. NSF has funded the CONVERGE initiative converge.colorado.edu Why CONVERGE? Why CONVERGE? • identify and coordinate researchers and research teams; • advance hazards and disaster research; • encourage the publication of data and data collection instruments and protocols (DesignSafe Cyberinfrastructure + CONVERGE). • support and accelerate training and mentoring; • fund virtual reconnaissance, field research, and the development of novel research instruments and data collection protocols; • accelerate the development of mobile applications for social science data collection (NHERI RAPID); Why CONVERGE? 2. NSF Supports Extreme Events Research (EER) Networks converge.colorado.edu Why the EER’s? Disciplinary -
P6.3 Using ERA40 in Cyclone Phase Space to Refine the Classification
P6.3 Using ERA40 in Cyclone Phase Space to Refine the Classification of Historical Tropical Storms Danielle Manning* and Robert Hart The Florida State University *Corresponding author email: [email protected] I. INTRODUCTION The goal of this study is to, when feasible Understanding of cyclone structural evolution within the ERA40 data, extend and refine the structural both during and beyond the tropical stage has increased characteristics of existing best-track cyclones. These tremendously over the past fifty years through various refinements may include the tropical or extratropical satellite-based, model-based, and analysis-based transition points in the lifecycle or the genesis point of classifications. This new knowledge has brought tropical cyclones that formed from cold-core origins. forward the reanalysis of historical storms in the context Finally, through a detailed examination of the full 45 of present understanding (Landsea et al. 2004) in order years, several cyclones were found of warm-core or to extend and revise the National Hurricane Center’s hybrid structure that may qualify for subtropical or (NHC) North Atlantic hurricane database (HURDAT; tropical status, but were not documented within the Neumann et al. 1993). This reanalysis is vital for the existing best-track archive. Case examples of all these filling of gaps within, and further improvement overall events are presented below, along with an evaluation of of the track and structural evolution of tropical cyclones. CPS intensity bias evolution over the ERA40 period. II. DATA AND METHODOLOGY Using ECMWF Reanalysis dataset (ERA40; Uppala et al. 2005), three parameters that classify a cyclone within a continuum of structure (warm to cold core, shallow to deep, and frontal to nonfrontal) can be calculated (Hart 2003).