Storm Surge Resilience and the Sendai Framework
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Abbreviations
Abbreviations A1B One of the IPCC SRES scenarios AIS Asociación Colombiana de Ingeniería ABM anti-ballistic missile Sísmica [Colombian Association for AA Auswärtiges Amt [Federal Ministry for Earthquake Engineering] Foreign Affairs, Germany] AKOM Afet Koordinasyon Merkezi [Istanbul ACOTA African Contingency Operations Training Metropolitan Municipality Disaster Assistance Coordination Centre] ACRS Arms Control and Regional Security AKP Adalet ve Kalkinma Partisi [Justice and ACSAD Arab Center for the Studies of Arid Zones Development Party] and Dry Lands AKUF AG Kriegsursachenforschung [Study Group ACSYS Arctic Climate System Study on the Causes of War] (at Hamburg ACUNU American Council for the United Nations University) University AL Arab League AD anno domini [after Christ] AMMA African Monsoon Multidisciplinary Analysis ADAM Adaptation and Mitigation Strategies: Project Supporting European Climate Policy (EU AMU Arab Maghreb Union funded project) An. 1 Annex 1 countries (under UNFCCC) ADB Asian Development Bank An. B Annex B countries (under Kyoto Protocol) ADRC Asian Disaster Reduction Centre ANAP Anavatan Partisi [Motherland Party] AESI Asociación Española de Ingeniría Sísmica ANU Australian National University [Association for Earthquake Engineering of AOSIS Alliance of Small Island States Spain] AP3A Early Warning and Agricultural Productions AfD African Development Bank Forecasting, project of AGRHYMET AFD Agence Française de Développement APEC Asia-Pacific Economic Cooperation AFED Arab Forum on Environment and APHES Assessing -
The East Coast Tidal Surge of 5 December 2013 Lincolnshire
OFFICIAL Lincolnshire’s Tidal Surge Response & Recovery ‘After Action’ Report The East Coast Tidal Surge of 5th December 2013 Lincolnshire Resilience Forum’s Response & Recovery ‘After Action’ Report 20th March 2014 1 OFFICIAL Lincolnshire’s Tidal Surge Response & Recovery ‘After Action’ Report Foreword On Thursday 5th December 2013 a deepening pressure system combined with high astronomical tides and strong to gale force ‘north westerly’ winds to generate a coastal surge along the whole of the east coast of England, the largest surge since the ‘great storm’ of 1953. Due to advances in surge forecasting, flood prediction and contingency planning at national, sub-national and local levels we were able to ‘get ahead’ of the storm. From Tuesday 3rd December partners began deploying one of the largest multi-agency emergency response and recovery operations ever conducted in Lincolnshire. This included the most significant evacuation operation in recent memory, the rescue of a number of people who became isolated by floodwaters, and work to ensure critical services were maintained and damaged infrastructure quickly repaired. Thankfully there were only 3 (relatively minor) casualties as a result of the surge, but more than 720 residential and commercial properties were inundated from the resultant overtopping and breach of defences. I would like to pass on my sympathy and support to those whose households and businesses flooded. We continue to work to support a full community recovery, and I commend the work of colleagues at Boston Borough Council who have led this work. In the circumstances this was a very good, forecast-led response and recovery effort. -
Historical Weather Data for Climate Risk Assessment
Historical Weather Data for Climate Risk Assessment Stefan Brönnimann1,2,*, Olivia Martius1,2,3, Christian Rohr1,4, David N. Bresch5,6 Kuan-Hui Elaine Lin7 1 Oeschger Centre for Climate Change Research, University of Bern, Switzerland 2 Institute of Geography, University of Bern, Switzerland 3 Mobiliar Lab for Natural Risks, University of Bern, Switzerland 4 Institute of History, University of Bern, Switzerland 5 Institute for Environmental Decisions, ETH Zurich, Universitätstrasse 22, 8092 Zurich, Switzerland 6 Federal Office of Meteorology and Climatology MeteoSwiss, Operation Center 1, P.O. Box 257, 8058 Zurich-Airport, Switzerland 7 Research Center for Environmental Changes, Academia Sinica, Taipei, Taiwan Revised submission to Annals of the New York Academy of Sciences * corresponding author: Stefan Brönnimann Institute of Geography, University of Bern Hallerstr. 12 CH-3012 Bern Switzerland [email protected] Short title: Historical Weather Data for Climate Risk Assessment Keywords: extreme events, climate risk, climate data, historical data | downloaded: 26.9.2021 Abstract. Weather and climate-related hazards are responsible for large monetary losses, material damages and societal consequences. Quantifying related risks is therefore an important societal task, particularly in view of future climate change. The past record of events plays a key role in this context. Historically, it was the only source of information and was maintained and passed on within cultures of memory. Today, new numerical techniques can again make use of historical weather data to simulate impacts quantitatively. In this paper we outline how historical environmental data can be used today in climate risk assessment by (i) developing and validating numerical model chains, (ii) providing a large statistical sample which can be directly exploited to estimate hazards and to model present risks, and (iii) establishing „worst-case“ events which are relevant references in the present or future. -
Village of Manchester Hazard Mitigation Plan Village of Manchester, Vermont
Village of Manchester Hazard Mitigation Plan , 2017 Village of Manchester, Vermont Table of Contents List of Tables ................................................................................................................................................. 2 List of Figures ................................................................................................................................................ 2 I. Introduction .......................................................................................................................................... 3 A. Purpose ............................................................................................................................................. 3 B. Mitigation Goals ................................................................................................................................ 3 II. Village Profile ........................................................................................................................................ 4 A. Regional Context ............................................................................................................................... 4 B. Demography and Land Use ............................................................................................................... 4 C. Economic and Cultural Resources ..................................................................................................... 4 D. Critical Facilities ............................................................................................................................... -
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. -
Economic Inequality and Institutional Adaptation in Response to Flood Hazards: a Historical Analysis
Copyright © 2018 by the author(s). Published here under license by the Resilience Alliance. van Bavel, B., D. R. Curtis, and T. Soens. 2018. Economic inequality and institutional adaptation in response to flood hazards: a historical analysis. Ecology and Society 23(4):30. https://doi.org/10.5751/ES-10491-230430 Research Economic inequality and institutional adaptation in response to flood hazards: a historical analysis Bas van Bavel 1, Daniel R. Curtis 2 and Tim Soens 3 ABSTRACT. To adequately respond to crises, adaptive governance is crucial, but sometimes institutional adaptation is constrained, even when a society is faced with acute hazards. We hypothesize that economic inequality, defined as unequal ownership of wealth and access to resources, crucially interacts with the way institutions function and are adapted or not. Because the time span for societal responses may be lengthy, we use the historical record as a laboratory to test our hypothesis. In doing so, we focus on floods and water management infrastructure. The test area is one where flood hazards were very evident—the Low Countries (present-day Netherlands and Belgium) in the premodern period (1300–1800)—and we employ comparative analysis of three regions within this geographical area. We draw two conclusions: first, both equitable and inequitable societies can demonstrate resilience in the face of floods, but only if the institutions employed to deal with the hazard are suited to the distributive context. Institutions must change parallel to any changes in inequality. Second, we show that institutional adaptation was not inevitable, but also sometimes failed to occur. Institutional adaptation was never inevitably triggered by stimulus of a hazard, but dependent on socio-political context. -
A User-Friendly Database of Coastal Flooding in The
www.nature.com/scientificdata OPEN A user-friendly database of coastal SUBJECT CATEGORIES » Environmental sciences flooding in the United Kingdom » Environmental social sciences from 1915–2014 » Physical oceanography Ivan D. Haigh1,2, Matthew P. Wadey1, Shari L. Gallop1, Heiko Loehr1, Robert J. Nicholls3, » Atmospheric dynamics Kevin Horsburgh4, Jennifer M. Brown4 & Elizabeth Bradshaw5 Coastal flooding caused by extreme sea levels can be devastating, with long-lasting and diverse consequences. Historically, the UK has suffered major flooding events, and at present 2.5 million properties and £150 billion of assets are potentially exposed to coastal flooding. However, no formal system is in place to catalogue which storms and high sea level events progress to coastal flooding. Furthermore, information Received: 19 January 2015 on the extent of flooding and associated damages is not systematically documented nationwide. Here we Accepted: 16 April 2015 present a database and online tool called ‘SurgeWatch’, which provides a systematic UK-wide record of Published: 12 May 2015 high sea level and coastal flood events over the last 100 years (1915-2014). Using records from the National Tide Gauge Network, with a dataset of exceedance probabilities and meteorological fields, SurgeWatch captures information of 96 storms during this period, the highest sea levels they produced, and the occurrence and severity of coastal flooding. The data are presented to be easily assessable and understandable to a range of users including, scientists, coastal engineers, managers and planners and concerned citizens. Design Type(s) observation design • data integration objective • time series design Measurement Type(s) oceanography Technology Type(s) data collection method Factor Type(s) Sample Characteristic(s) coast • England • Wales • British Isles • Scotland 1Ocean and Earth Science, National Oceanography Centre, University of Southampton, European Way, Southampton SO14 3ZH, UK. -
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. -
Flooding After Storm Desmond PERC UK 2015 Flooding in Cumbria After Storm Desmond PERC UK 2015
Flooding after Storm Desmond PERC UK 2015 Flooding in Cumbria after Storm Desmond PERC UK 2015 The storms that battered the north of England and parts of Scotland at the end of 2015 and early 2016 caused significant damage and disruption to families and businesses across tight knit rural communities and larger towns and cities. This came just two years after Storm Xaver inflicted significant damage to the east coast of England. Flooding is not a new threat to the residents of the Lake District, but the severity of the events in December 2015 certainly appears to have been regarded as surprising. While the immediate priority is always to ensure that defence measures are overwhelmed. We have also these communities and businesses are back up on their looked at the role of community flood action groups feet as quickly and effectively as possible, it is also in the response and recovery from severe flooding. important that all those involved in the response take Our main recommendations revolve around three key the opportunity to review their own procedures and themes. The first is around flood risk communication, actions. It is often the case that when our response is including the need for better communication of hazard, put to the test in a ‘real world’ scenario that we risk and what actions to take when providing early discover things that could have been done better, or warning services to communities. The second centres differently, and can make changes to ensure continuous around residual risk when the first line of flood improvement. This is true of insurers as much as it is of defences, typically the large, constructed schemes central and local government and the emergency protecting entire cities or areas, are either breached services, because events like these demand a truly or over-topped. -
Supplement of Storm Xaver Over Europe in December 2013: Overview of Energy Impacts and North Sea Events
Supplement of Adv. Geosci., 54, 137–147, 2020 https://doi.org/10.5194/adgeo-54-137-2020-supplement © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Supplement of Storm Xaver over Europe in December 2013: Overview of energy impacts and North Sea events Anthony James Kettle Correspondence to: Anthony James Kettle ([email protected]) The copyright of individual parts of the supplement might differ from the CC BY 4.0 License. SECTION I. Supplement figures Figure S1. Wind speed (10 minute average, adjusted to 10 m height) and wind direction on 5 Dec. 2013 at 18:00 GMT for selected station records in the National Climate Data Center (NCDC) database. Figure S2. Maximum significant wave height for the 5–6 Dec. 2013. The data has been compiled from CEFAS-Wavenet (wavenet.cefas.co.uk) for the UK sector, from time series diagrams from the website of the Bundesamt für Seeschifffahrt und Hydrolographie (BSH) for German sites, from time series data from Denmark's Kystdirektoratet website (https://kyst.dk/soeterritoriet/maalinger-og-data/), from RWS (2014) for three Netherlands stations, and from time series diagrams from the MIROS monthly data reports for the Norwegian platforms of Draugen, Ekofisk, Gullfaks, Heidrun, Norne, Ormen Lange, Sleipner, and Troll. Figure S3. Thematic map of energy impacts by Storm Xaver on 5–6 Dec. 2013. The platform identifiers are: BU Buchan Alpha, EK Ekofisk, VA? Valhall, The wind turbine accident letter identifiers are: B blade damage, L lightning strike, T tower collapse, X? 'exploded'. The numbers are the number of customers (households and businesses) without power at some point during the storm. -
Understanding Music Past and Present
Understanding Music Past and Present N. Alan Clark, PhD Thomas Heflin, DMA Jeffrey Kluball, EdD Elizabeth Kramer, PhD Understanding Music Past and Present N. Alan Clark, PhD Thomas Heflin, DMA Jeffrey Kluball, EdD Elizabeth Kramer, PhD Dahlonega, GA Understanding Music: Past and Present is licensed under a Creative Commons Attribu- tion-ShareAlike 4.0 International License. This license allows you to remix, tweak, and build upon this work, even commercially, as long as you credit this original source for the creation and license the new creation under identical terms. If you reuse this content elsewhere, in order to comply with the attribution requirements of the license please attribute the original source to the University System of Georgia. NOTE: The above copyright license which University System of Georgia uses for their original content does not extend to or include content which was accessed and incorpo- rated, and which is licensed under various other CC Licenses, such as ND licenses. Nor does it extend to or include any Special Permissions which were granted to us by the rightsholders for our use of their content. Image Disclaimer: All images and figures in this book are believed to be (after a rea- sonable investigation) either public domain or carry a compatible Creative Commons license. If you are the copyright owner of images in this book and you have not authorized the use of your work under these terms, please contact the University of North Georgia Press at [email protected] to have the content removed. ISBN: 978-1-940771-33-5 Produced by: University System of Georgia Published by: University of North Georgia Press Dahlonega, Georgia Cover Design and Layout Design: Corey Parson For more information, please visit http://ung.edu/university-press Or email [email protected] TABLE OF C ONTENTS MUSIC FUNDAMENTALS 1 N. -
Open Domain Factoid Question Answering Systems
OPEN DOMAIN FACTOID QUESTION ANSWERING SYSTEM TEK YANITLI SORULAR İÇİN AÇIK ALANLI SORU YANITLAMA SİSTEMİ Farhad SOLEIMANIAN GHAREHCHOPOGH Prof.Dr. İlyas ÇİÇEKLİ Supervisor Submitted to Institute of Graduate School in Science and Engineering of Hacettepe University as a Partial Fulfillment to the Requirements for the Award of the Degree of Doctor of Philosophy in Computer Engineering 2015 ETHICS In this thesis study, prepared in accordance with the spelling rules of Institute of Graduate School in Science and Engineering of Hacettepe University, I declare that all the information and documents have been obtained in the base of the academic rules all audio-visual and written information and results have been presented according to the rules of scientific ethics in case of using other Works, related studies have been cited in accordance with the scientific standards all cited studies have been fully referenced I did not do any distortion in the data set And any part of this thesis has not been presented as another thesis study at this or any other university. 10 September 2015 FARHAD SOLEIMANIAN GHAREHCHOPOGH ABSTRACT OPEN DOMAIN FACTOID QUESTION ANSWERING SYSTEM Farhad SOLEIMANIAN GHAREHCHOPOGH Doctor of Philosophy, Department of Computer Engineering Supervisor: Prof.Dr. İlyas ÇİÇEKLİ September 2015, 237 pages Question Answering (QA) is a field of Artificial Intelligence (AI) and Information Retrieval (IR) and Natural Language Processing (NLP), and leads to generating systems that answer to questions natural language in open and closed domains, automatically. Question Answering Systems (QASs) have to deal different types of user questions. While answers for some simple questions can be short phrases, answers for some more complex questions can be short texts.