How Our Decisions Are Shaping Future Disaster Risk Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized

Total Page:16

File Type:pdf, Size:1020Kb

How Our Decisions Are Shaping Future Disaster Risk Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized The making of a riskier Public Disclosure Authorized future: How our decisions are shaping future disaster risk Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized The making of a riskier future: How our decisions are shaping future disaster risk © 2016 Global Facility for Disaster Reduction and Recovery 1818 H Street, N.W., Washington, D.C., 20433, U.S.A. The text in this publication may be reproduced in whole or in part and in any form for educational or nonprofit uses, without special permission, provided acknowledgement of the source is made. The GFDRR Secretariat would appreciate receiving a copy of any publication that uses this report as a source. Copies may be sent to the GFDRR Secretariat at the above address. No use of this publication may be made for resale or other commercial purpose without prior written consent of the GFDRR Secretariat. All images remain the sole property of the source and may not be used for any purpose without written permission from the source. Notes: Fiscal year (FY) runs from July 1 to June 30; the financial contributions and expenditures reported are reflected up to June 30, 2015; all dollar amounts are in US dollars ($) unless otherwise indicated. The World Bank does not guarantee the accuracy of the data included in this work. The boundaries, colors, denominations, and other information shown on any map in this work do not imply any judgment on the part of The World Bank concerning the legal status of any territory or the endorsement or acceptance of such boundaries. Design: Miki Fernández/ULTRAdesigns, Inc. Cover: Kathmandu cityscape, Nepal. Photo credit: sagarmanis/Thinkstock.com; Inside cover: Bhaktapur, Nepal – May 9, 2015: Woman outside her earthquake-ruined house in Bhaktapur, Nepal, located 30 km east of Kathmandu. The town was once rich with Buddhist and Hindu temples and a popular tourist spot for those visiting Kathmandu. Photo credit: Jules2013/Thinkstock.com Table of Contents Foreword vii Acknowledgments ix Abbreviations x Executive Summary/Overview xiii 1. INTRODUCTION 1 2. DISASTER RISK 5 3. DRIVERS OF EVOLVING DISASTER RISK: HAZARD 9 Hydrometeorological hazards 9 Tropical cyclone 10 Extratropical cyclone 12 Flooding 13 Extreme heat 17 Drought 18 Wildfire 19 Geotechnical and geophysical hazards 20 Seismic and volcanic hazard 20 Landslide 20 4. DRIVERS OF EVOLVING DISASTER RISK: EXPOSURE 23 Population growth 24 Increased socioeconomic activity 28 Land-use change 28 Data on evolving exposure 28 5. DRIVERS OF EVOLVING DISASTER RISK: VULNERABILITY 31 Structural vulnerability 31 Social vulnerability 33 iv 6. QUANTIFYING THE EVOLUTION OF DISASTER RISK 37 Simple or complex approach 39 Modeling interrelated and evolving hazards 40 Multiple influences on coastal flood risk 40 Time dependency 41 Uncertainty in risk assessment 42 Hazard uncertainty 42 Use of climate projections in disaster risk assessment 42 Uncertainty in exposure data and projections 44 Producing detailed risk assessments 46 Complexities in modeling evolving exposure 49 Using socioeconomic scenarios to project population 49 Projecting urban expansion 51 Evolving vulnerability: An ongoing challenge 53 7. IDENTIFYING EFFECTIVE POLICIES FOR A RESILIENT FUTURE 59 Mitigate climate change 60 Manage urbanization 60 Limit harmful land-use change and resource consumption 60 Control increases in exposure 60 Reduce vulnerability through urban design 61 Manage risk through construction 62 Building practices 62 Continuing habitability of structures 64 Consider ecosystem-based risk management 65 Improve data for risk modeling 66 Dynamic exposure and vulnerability data 66 High-resolution elevation data 66 Flood protection data 67 Implement robust, flexible adaptation 67 Enhance disaster resilience 68 Plan recovery and reconstruction before the event 69 REFERENCES 70 v 8. CASE STUDIES 81 Case Study A. World Weather Attribution 81 Case Study B. Using Catastrophe Models to Assess Future Risk 86 Case Study C. Sinking Cities: An Integrated Approach to Solutions 90 Case Study D. The Evolving Risk of Earthquakes: Past, Present, and Future 101 Case Study E. Changing Earthquake Vulnerability Linked to Informal Building Expansion 109 Case Study F. An Interrelated Hazards Approach to Anticipating Evolving Risk 114 Case Study G. Evolution of Risk in Eastern Europe and Central Asia 122 Case Study H. Open Data and Dynamic Understandings of Risk 129 Case Study I. Science Influencing Land-Use Policy: A Story from New Zealand 135 vii Foreword Tomorrow’s risk is being built today. We must therefore move away from risk assessments that show risk at a single point in the present and move instead towards risk assessments that can guide decision makers towards a resilient future. atural disasters can have truly global impacts. this goal, we need to strengthen policies and actions that There is evidence that approximately 75,000 years enable us to support larger populations, increased asset Nago, after the Toba volcano erupted in Sumatra, wealth, and more urbanized countries without increased Indonesia, a global volcanic winter may have decimated disaster risk. the global human population to just several thousand. Tomorrow’s risk is being built today. We must therefore Since then, natural hazards have frequently affected move away from risk assessments that show risk at a communities on scales large and small, but civilization as single point in the present—which can quickly become a whole is more likely to survive a catastrophe today than outdated—and move instead towards risk assessments ever before. That is the good news. that can guide decision makers towards a resilient future. The disturbing news is that the impacts of natural Only then will they be able to visualize the potential risk disasters have been growing rapidly due to global that results from their decisions taken today, and see the population growth, urbanization and increased benefit of enacting policies to reduce climate change, socioeconomic activity—with a tenfold increase in losses halt the construction of unsafe buildings, enforce land from disasters since the 1970s. Moreover, these numbers use plans, reduce subsidence, and more. have yet to incorporate the real impact of climate We have more than 75,000 years of experience living change. By the end of the century, coastal areas will see with disasters, but today’s challenges demand that we do more frequent and intense inundation due to sea level things differently. We must continually learn, innovate, rise, and changes in rainfall patterns will trigger more and push boundaries, so that we can build a safer world frequent droughts and floods, putting many lives and for ourselves and the generations to come. livelihoods in jeopardy. In 2015, world leaders made a commitment in Sendai, Japan to reduce the number of people affected, the direct Francis Ghesquiere economic loss, and the damage to critical infrastructure Head, Global Facility for Disaster Reduction and basic services from disasters by 2030. To achieve and Recovery FACING PAGE Neena Sasaki, 5, carries some of the family belongings from her home that was destroyed after the devastating earthquake and tsunami on March 15, 2011 in Rikuzentakata, Miyagi province, Japan. Photo credit: Paula Bronstein/Thinkstock.com viii / Making a riskier future: How our decisions are shaping future disaster risk ix Acknowledgments his publication was prepared by a team comprising College London Hazard Centre); Gilles Erkens (Deltares Stuart Fraser, Brenden Jongman, Simone Balog, Research Institute); Alexandra Guerrero (RMS); David TAlanna Simpson, Keiko Saito, and Anne Himmelfarb. Karoly (ARC Centre of Excellence for Climate System Science, University of Melbourne); Christopher Kilburn Valuable review of the publication was provided by (University College London Hazard Centre); Andrew King Rashmin Gunasekera (World Bank), Stéphane Hallegatte (ARC Centre of Excellence for Climate System Science, (World Bank), Federica Rangieri (World Bank), and University of Melbourne); Anne Kiremidjian (Stanford Maarten van Aalst (Red Cross/Red Crescent Climate University); David Lallemant (Stanford University); John Centre; International Research Institute for Climate and Lambert (Deltares Research Institute); Catherine Linard Society). (Université Libre de Bruxelles); Hiro Miyazaki (University Case study contributors include Axis Maps LLC; James of Tokyo); Richard Murnane (Global Facility for Disaster Beban (GNS Science); Tom Bucx (Deltares Research Reduction and Recovery [GFDRR]); Geert Jan van Institute); Zach Bullock (Stanford University); Henry Oldenborgh (Royal Netherlands Meteorological Institute); Burton (Stanford University); Luis Ceferino (Stanford Friederike Otto (Environmental Change Institute, University); Erin Coughlan de Perez (Red Cross/Red University of Oxford); Wendy Saunders (GNS Science); Crescent Climate Centre; Institute for Environmental Roop Singh (Red Cross/Red Crescent Climate Centre); Studies, VU University; International Research Institute Dina Sperling (Climate Central); Robert Soden (GFDRR); for Climate and Society); Kate Crowley (National Institute Annegien Tjissen (GFDRR); Joaquin Toro (GFDRR); John of Water and Atmospheric Research Ltd.); Heidi Cullen Twigg (Centre for Urban Sustainability and Resilience, (Climate Central); Rien Dam (WaterLand Experts); University College London); Maarten van Aalst (Red James Daniell (Karlsruhe Institute of Technology); Cross/Red Crescent Climate Centre; International Ger de Lange (Deltares Research
Recommended publications
  • Analisa Pengaruh Letusan Abu Vulkanik Gunung Marapi Di Sumatera Barat
    Agusta Kurniawan. : Analisa Pengaruh Letusan Abu Vulkanik Gunung Marapi di Sumatera Barat ... ANALISA PENGARUH LETUSAN ABU VULKANIK GUNUNG MARAPI DI SUMATERA BARAT TERHADAP PENGUKURAN GAS (SO2) DAN PARTIKEL (PM10 DAN SPM) DI STASIUN PEMANTAU ATMOSFER GLOBAL BUKIT KOTOTABANG THE ANALYSIS OF EFFECT OF THE INFLUNCE OF MARAPI VOLCANIC ERUPTION IN WEST SUMATRA TO THE MEASUREMENT OF GAS (SO2) AND PARTICULATE MTTER (PM10 AND SPM) IN GLOBAL ATMOSPHERIC MONITORING KOTOTABANG HILL STATION Agusta Kurniawan1 (Diterima tanggal 15-11-2011; Disetujui tanggal 14-03-2012) ABSTRAK Tujuan penelitian ini adalah untuk melakukan analisa pengaruh letusan abu vulkanik Gunung Marapi di Sumatera Barat pada awal bulan Agustus 2011 terhadap pengukuran gas (SO2) dan partikel (PM10 dan SPM) di SPAG Bukit Kototabang. Sebagai data pembanding yaitu data rata-rata harian sebelum letusan abu vulkanik gunung Marapi, yaitu data harian bulan Juli 2011, sedangkan sebagai data sampel (data setelah Gunung Marapi meletus) digunakan data rata-rata harian 1-10 Agustus 2011. Model Hysplit Volcanic Ash dari NOAA (National Oceanic and Atmospheric Administration) dan Citra Satelit OMI (Ozon Monitoring Instrument) digunakan untuk memperkirakan arah letusan Gunung Marapi. Hasil analisis menunjukkan bahwa letusan abu vulkanik Gunung Marapi pada awal Agustus 2011 tidak berpengaruh terhadap pengukuran pengukuran gas (SO2) dan partikel (PM10 dan SPM) di Stasiun Pemantau Atmosfer Global Bukit Kototabang. Kata Kunci: Gunung Marapi, SPAG Bukit Kototabang, SO2, PM10 dan SPM, Hysplit Volcanic Ash Model ABSTRACT The purpose of this study was to analyze the influence of volcanic ash eruption of Mount Marapi in West Sumatra in early August 2011 to the measurement of gas (SO2) and particulate matter (PM10 and SPM) in Global GAW Bukit Kototabang Station.
    [Show full text]
  • Natural Disasters in the Middle East and North Africa
    Natural Disasters in Public Disclosure Authorized the Middle East and North Africa: A Regional Overview Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized January 2014 Urban, Social Development, and Disaster Risk Management Unit Sustainable Development Department Middle East and North Africa Natural Disasters in the Middle East and North Africa: A Regional Overview © 2014 The International Bank for Reconstruction and Development / The World Bank 1818 H Street NW Washington DC 20433 Telephone: 202-473-1000 Internet: www.worldbank.org All rights reserved 1 2 3 4 13 12 11 10 This volume is a product of the staff of the International Bank for Reconstruction and Development / The World Bank. The findings, interpretations, and conclusions expressed in this volume do not necessarily reflect the views of the Executive Directors of The World Bank or the governments they represent. The World Bank does not guarantee the accuracy of the data included in this work. The boundar- ies, colors, denominations, and other information shown on any map in this work do not imply any judgment on the part of The World Bank concerning the legal status of any territory or the endorse- ment or acceptance of such boundaries. Rights and Permissions The material in this publication is copyrighted. Copying and/or transmitting portions or all of this work without permission may be a violation of applicable law. The International Bank for Recon- struction and Development / The World Bank encourages dissemination of its work and will normally grant permission to reproduce portions of the work promptly. For permission to photocopy or reprint any part of this work, please send a request with complete information to the Copyright Clearance Center Inc., 222 Rosewood Drive, Danvers, MA 01923, USA; telephone: 978-750-8400; fax: 978-750-4470; Internet: www.copyright.com.
    [Show full text]
  • Global Catastrophic Risks 2016
    Global Challenges Foundation Global Catastrophic Risks 2016 © Global Challenges Foundation/Global Priorities Project 2016 GLOBAL CATASTROPHIC RISKS 2016 THE GLOBAL CHALLENGES FOUNDATION works to raise awareness of the The views expressed in this report are those of the authors. Their Global Catastrophic Risks. Primarily focused on climate change, other en- statements are not necessarily endorsed by the affiliated organisations. vironmental degradation and politically motivated violence as well as how these threats are linked to poverty and rapid population growth. Against this Authors: background, the Foundation also works to both identify and stimulate the Owen Cotton-Barratt*† development of good proposals for a management model – a global gover- Sebastian Farquhar* nance – able to decrease – and at best eliminate – these risks. John Halstead* Stefan Schubert* THE GLOBAL PRIORITIES PROJECT helps decision-makers effectively prior- Andrew Snyder-Beattie† itise ways to do good. We achieve his both by advising decision-makers on programme evaluation methodology and by encouraging specific policies. We * = The Global Priorities Project are a collaboration between the Centre for Effective Altruism and the Future † = The Future of Humanity Institute, University of Oxford of Humanity Institute, part of the University of Oxford. Graphic design: Accomplice/Elinor Hägg Global Challenges Foundation in association with 4 Global Catastrophic Risks 2016 Global Catastrophic Risks 2016 5 Contents Definition: Global Foreword 8 Introduction 10 Catastrophic Risk Executive summary 12 1. An introduction to global catastrophic risks 20 – risk of events or 2. What are the most important global catastrophic risks? 28 Catastrophic climate change 30 processes that would Nuclear war 36 Natural pandemics 42 Exogenous risks 46 lead to the deaths of Emerging risks 52 Other risks and unknown risks 64 Our assessment of the risks 66 approximately a tenth of 3.
    [Show full text]
  • Welcome to the Heaven of Specialty Coffee
    Coffee Quotes INDONESIA “ I have measured out my life with coffee spoons. ” (T. S. Eliot) “ If I asked for a cup of coffee, EDITION someone would search for the double meaning. ” (Mae West) “ To me, the smell of fresh-made coffee is one Trade•Tourism•Investment FIRST of the greatest inventions. ” (Hugh Jackman) “ The ability to deal with people is as purchasable a commodity as sugar or coffee and I will pay more for that ability than for any other under the sun. ” Welcome to The Heaven (John D. Rockefeller) “ Coffee is a language in itself. ” of Specialty Coffee (Jackie Chan) “ I like cappuccino, actually. But even a bad cup of coffee is better than no coffee at all. ” (David Lynch) “ If it wasn't for the coffee, I'd have no identifiable personality whatsover. “ (David Letterman) :” Good communication is as stimulating as black coffee, and just as hard. ” (Anne Spencer) “ I would rather suffer with coffee than be senseless. “ (Napoleon Bonaparte) “ Coffee, the favourite drink of civilize world. ” (Thomas Jefferson) “ What on earth could be more luxurious than a sofa, a book and a cup of coffee? “ (Anthony Troloppe) “Coffee is far more than a beverage. It is an invitation to life, (Foto: web/edit) disguised as a cup of warm liquid. It’s a trumpet wakeup call or a gentle rousing hand on your shoulder… Coffee is an experience, an offer, a rite of passage, a good excuse to get together. ” (Nichole Johnson) “ A guy’s gotta live, you know, gotta make his way and find his Exotic & Unique Indonesian Coffee meaning in life and love, and to do that he needs coffee, he needs coffee and coffee and coffee.
    [Show full text]
  • Exposure and Vulnerability
    Determinants of Risk: 2 Exposure and Vulnerability Coordinating Lead Authors: Omar-Dario Cardona (Colombia), Maarten K. van Aalst (Netherlands) Lead Authors: Jörn Birkmann (Germany), Maureen Fordham (UK), Glenn McGregor (New Zealand), Rosa Perez (Philippines), Roger S. Pulwarty (USA), E. Lisa F. Schipper (Sweden), Bach Tan Sinh (Vietnam) Review Editors: Henri Décamps (France), Mark Keim (USA) Contributing Authors: Ian Davis (UK), Kristie L. Ebi (USA), Allan Lavell (Costa Rica), Reinhard Mechler (Germany), Virginia Murray (UK), Mark Pelling (UK), Jürgen Pohl (Germany), Anthony-Oliver Smith (USA), Frank Thomalla (Australia) This chapter should be cited as: Cardona, O.D., M.K. van Aalst, J. Birkmann, M. Fordham, G. McGregor, R. Perez, R.S. Pulwarty, E.L.F. Schipper, and B.T. Sinh, 2012: Determinants of risk: exposure and vulnerability. In: Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation [Field, C.B., V. Barros, T.F. Stocker, D. Qin, D.J. Dokken, K.L. Ebi, M.D. Mastrandrea, K.J. Mach, G.-K. Plattner, S.K. Allen, M. Tignor, and P.M. Midgley (eds.)]. A Special Report of Working Groups I and II of the Intergovernmental Panel on Climate Change (IPCC). Cambridge University Press, Cambridge, UK, and New York, NY, USA, pp. 65-108. 65 Determinants of Risk: Exposure and Vulnerability Chapter 2 Table of Contents Executive Summary ...................................................................................................................................67 2.1. Introduction and Scope..............................................................................................................69
    [Show full text]
  • Anjeski, Paul OH133
    Wisconsin Veterans Museum Research Center Transcript of an Oral History Interview with PAUL ANJESKI Human Resources/Psychologist, Navy, Vietnam War Era 2000 OH 133 1 OH 133 Anjeski, Paul, (1951- ). Oral History Interview, 2000. User Copy: 1 sound cassette (ca. 84 min.); analog, 1 7/8 ips, mono. Master Copy: 1 sound cassette (ca. 84 min.); analog, 1 7/8 ips, mono. Video Recording: 1 videorecording (ca. 84 min.); ½ inch, color. Transcript: 0.1 linear ft. (1 folder). Abstract: Paul Anjeski, a Detroit, Michigan native, discusses his Vietnam War era experiences in the Navy, which include being stationed in the Philippines during social unrest and the eruption of Mount Pinatubo. Anjeski mentions entering ROTC, getting commissioned in the Navy in 1974, and attending Damage Control Officer School. He discusses assignment to the USS Hull as a surface warfare officer and acting as navigator. Anjeski explains how the Hull was a testing platform for new eight-inch guns that rattled the entire ship. After three and a half years aboard ship, he recalls human resources management school in Millington (Tennessee) and his assignment to a naval base in Rota (Spain). Anjeski describes duty as a human resources officer and his marriage to a female naval officer. He comments on transferring to the Naval Reserve so he could attend graduate school and his work as part of a Personnel Mobilization Team. He speaks of returning to duty in the Medical Service Corps and interning as a psychologist at Bethesda Hospital (Maryland), where his duties included evaluating people for submarine service, trauma training, and disaster assistance.
    [Show full text]
  • Technical Deep Dive on Deep Dive Technical Summary Report Summary
    TECHNICAL DEEP DIVE ON SEISMIC RISK AND RESILIENCE - SUMMARY REPORT SUMMARY - RESILIENCE AND RISK SEISMIC ON DIVE DEEP TECHNICAL TECHNICAL DEEP DIVE ON AND SUMMARY REPORT This report was prepared by World Bank staff. The findings, interpretations, and conclusions expressed here do not necessarily reflect the views of The World Bank, its Board of Executive Directors, or the governments they represent. The World Bank does not guarantee the accuracy of the data included in this work. The boundaries, colors, denominations, and other information shown on any map in this work do not imply any judgment on the part of the World Bank concerning the legal status of any territory or the endorsement or acceptance of such boundaries. Rights and Permissions: The World Bank encourages dissemination of its knowledge, this work may be reproduced, in whole or in part, for noncommercial purposes as long as full attribution to the work is given. The material in this work is subject to copyright. © 2018 International Bank for Reconstruction and Development / International Development Association or The World Bank 1818 H Street NW Washington DC 20433 Cover image: Varunyuuu/Shutterstock.com TECHNICAL DEEP DIVE (TDD) ON SEISMIC RISK AND RESILIENCE MARCH 12–16, 2018 This Technical Deep Dive (TDD) was jointly organized by the World Bank Disaster Risk Management (DRM) Hub, Tokyo, and the Tokyo Development Learning Center (TDLC), in partnership with the Government of Japan (the Ministry of Finance; the Cabinet Office; the Ministry of Land, Infrastructure, Transport and Tourism [MLIT]; the Japan International Cooperation Agency [JICA]; the Japan Meteorological Agency [JMA]; Sendai City; and Kobe City).
    [Show full text]
  • Catastrophism, Natural Disasters, and Cultural Change John Grattan and Robin Torrence
    Theme: Archaeology and the Environment Symposium 017/1 Grattan & Torrence Symposium: Catastrophism, Natural Disasters, and Cultural Change John Grattan and Robin Torrence The aim of this session is to examine both the short and long-term consequences of extreme natural events on patterns of cultural change. Archaeological theory about the pace and character of cultural change generally focuses on processes which are internally generated and which unfold slowly through time. Since environmental determinism has fallen out of favour, theories about social evolution pay very little attention to external, nonhuman factors nor to random factors. Little or no consideration has been given to the effects of one-off natural disasters. In contrast, a number of theoretical perspectives involving catastrophism, chaos, punctuated evolution, etc. provide a range of alternative views that focus on the effects of random events. One of the goals of the symposium is to assess the value of these theories for explaining the impacts of natural disasters on cultural change. Through extended discussions following short presentations of case studies representing a very broad coverage in spatial, chronological and cultural terms, the participants will consider a range of general questions. How and in what ways do natural hazards affect human societies? Have natural disasters played an important role in human evolution? Do natural disasters have only short-term, limited effects or should they play an important role within general theories about cultural change and
    [Show full text]
  • Nahdhatul Ulama: from Traditionalist to Modernist Anzar Abdullah
    Nahdhatul Ulama: from traditionalist to modernist Anzar Abdullah, Muhammad Hasbi & Harifuddin Halim Universitas Islam Makassar Universitas Bosowa (UNIBOS) Makassar [email protected] Abstract This article is aimed to discuss the change shades of thought in Nahdhatul Ulama (NU) organization, from traditionalist to modernist. This is a literature study on thought that develop within related to NU bodies with Islamic cosmopolitanism discourse for interact and absorb of various element manifestation cultural and insight scientist as a part from discourse of modernism. This study put any number figures of NU as subject. The results of the study show that elements thought from figure of NU, like Gusdur which includes effort eliminate ethnicity, strength plurality culture, inclusive, liberal, heterogeneity politics, and life eclectic religion, has been trigger for the birth of the modernism of thought in the body of NU. It caused change of religious thought from textual to contextual, born in freedom of thinking atmosphere. Keywords: Nahdhatul Ulama, traditionalist, modernist, thought, organization Introduction The dynamic of Islamic thought that continues to develop within the NU organization in the present context, it is difficult to say that NU is still traditional, especially in the area of religious thought. This can be seen in the concept of inclusivism, cosmopolitanism, and even liberalism developed by NU figures such as Abdurrahman Wahid, Achmad Siddiq, and some young NU figures, such as Ulil Absar Abdalla. This shows a manifestation of modern thought. Critical thinking as a feature of modernism seems to have become the consumption of NU activists today. Therefore, a new term emerged among those called "re- interpretation of ahlussunah-waljamaah" and the re-interpretation of the concept of "bermazhab" or sect.
    [Show full text]
  • How to Stop a Supervolcano
    HOW TO STOP A SUPERVOLCANO [VIDEO TRANSCRIPT] In 1816, red snow fell in Maryland. And brown snow. And blue snow.1 Which was kind of weird. Even weirder? It was May. Parts of Pennsylvania were covered in half an inch of ice … in July.2 1816 was known as “The Year Without a Summer.” And the phenomenon wasn’t limited to the U.S. In fact, the reason Americans were shivering in the middle of the year … had to do with something that happened half a world away. The darkened, hazy skies produced by “The Year Without a Summer” led to a series of famous paintings by the likes of J.M.W. Turner, Caspar David Friedrich, and John Crome. Modern audiences often believe that the use of lighting in these works is stylized, not realizing that it was a reflection of the actual conditions at the time. Another artistic legacy of the year without a summer: Mary Shelley and her summer vacation companions at Lake Geneva were forced indoors, where they entertained each other by coming up with horror stories. Shelley’s contribution eventually became Frankenstein. The eruption of the volcano at Mount Tambora in Indonesia had released a massive cloud of ash and sulfur dioxide into the stratosphere. As a result, temperatures in the Northern Hemisphere plummeted. Crops failed and livestock died en masse. Between the eruption itself, the ensuing tsunamis, and the resulting starvation, approximately 92,000 people died.3 It is widely regarded as the worst volcanic eruption in recorded history. Here’s the good news: you didn’t have to live through it.
    [Show full text]
  • Assessing the Impact of a Future Volcanic Eruption on Decadal Predictions
    Earth Syst. Dynam., 9, 701–715, 2018 https://doi.org/10.5194/esd-9-701-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Assessing the impact of a future volcanic eruption on decadal predictions Sebastian Illing1, Christopher Kadow1, Holger Pohlmann2, and Claudia Timmreck2 1Freie Universität Berlin, Institute of Meteorology, Berlin, Germany 2Max Planck Institute for Meteorology, Hamburg, Germany Correspondence: Sebastian Illing ([email protected]) Received: 22 January 2018 – Discussion started: 2 February 2018 Accepted: 27 April 2018 – Published: 6 June 2018 Abstract. The likelihood of a large volcanic eruption in the future provides the largest uncertainty concerning the evolution of the climate system on the timescale of a few years, but also an excellent opportunity to learn about the behavior of the climate system, and our models thereof. So the following question emerges: how predictable is the response of the climate system to future eruptions? By this we mean to what extent will the volcanic perturbation affect decadal climate predictions and how does the pre-eruption climate state influence the impact of the volcanic signal on the predictions? To address these questions, we performed decadal forecasts with the MiKlip prediction system, which is based on the MPI-ESM, in the low-resolution configuration for the initialization years 2012 and 2014, which differ in the Pacific Decadal Oscillation (PDO) and North Atlantic Oscillation (NAO) phase. Each forecast contains an artificial Pinatubo-like eruption starting in June of the first prediction year and consists of 10 ensemble members. For the construction of the aerosol radiative forcing, we used the global aerosol model ECHAM5-HAM in a version adapted for volcanic eruptions.
    [Show full text]
  • Radiative and Climate Impacts of a Large Volcanic Eruption During Stratospheric Sulfur Geoengineering
    Atmos. Chem. Phys., 16, 305–323, 2016 www.atmos-chem-phys.net/16/305/2016/ doi:10.5194/acp-16-305-2016 © Author(s) 2016. CC Attribution 3.0 License. Radiative and climate impacts of a large volcanic eruption during stratospheric sulfur geoengineering A. Laakso1, H. Kokkola1, A.-I. Partanen2,3, U. Niemeier4, C. Timmreck4, K. E. J. Lehtinen1,5, H. Hakkarainen6, and H. Korhonen2 1Finnish Meteorological Institute, Atmospheric Research Centre of Eastern Finland, Kuopio, Finland 2Finnish Meteorological Institute, Climate Research, Helsinki, Finland 3Department of Geography, Planning and Environment, Concordia University, Montréal, Québec, Canada 4Max Planck Institute for Meteorology, Hamburg, Germany 5Department of Applied Physics, University of Eastern Finland, Kuopio campus, Kuopio, Finland 6A. I. Virtanen Institute for Molecular Sciences, University of Eastern Finland, Kuopio, Finland Correspondence to: A. Laakso (anton.laakso@fmi.fi) Received: 18 June 2015 – Published in Atmos. Chem. Phys. Discuss.: 12 August 2015 Revised: 21 December 2015 – Accepted: 22 December 2015 – Published: 18 January 2016 Abstract. Both explosive volcanic eruptions, which emit sul- ulation, only about one-third of the global ensemble-mean fur dioxide into the stratosphere, and stratospheric geoengi- cooling occurs after the eruption, compared to that occur- neering via sulfur injections can potentially cool the climate ring after an eruption under unperturbed atmospheric con- by increasing the amount of scattering particles in the at- ditions. Furthermore, the global cooling signal is seen only mosphere. Here we employ a global aerosol-climate model for the 12 months after the eruption in the former scenario and an Earth system model to study the radiative and climate compared to over 40 months in the latter.
    [Show full text]