Case Study on Sea-Level Rise Impacts
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Sustainable Mediterranean, Issue No 78
ISSUE 78 Sustainable Mediterranean MEDITERRANEE DURABLE I BIΩΣIMH MEΣOΓEIOΣ I MEDITERRANEO SOSTENIBLE I Climate Change: The rapidly increasing challenge for the Mediterranean 1 SUSTAINABLE MEDITERRANEAN | ISSUE 78 Guest Editor’s Corner As dawn rose over snow-covered Kyoto, (Japan) degree of risk of overstepping the 1.5°C limit – a 2100 – with the ‘collapse of civilisation as we actions - casting a shadow of doubt on prospects sleep-deprived delegates, observers and my fel- level which would limit the risk of giving certain know it’ foreseen some time before that. for a successful COP 26 outcome. low journalists cheered and clapped as the fi- Earth tipping points an additional push. Needed nal all-night session of the UN Framework Con- emission cuts will not only require a decarboni- The UK-hosted ‘live’ COP 26 in Glasgow this No- If urgent comprehensive global action is essen- vention on Climate Change’s COP3 (December sation revolution - by phasing out fossil energy vember (with doubts persisting whether the UK tial, so by definition are its components - region- 1997) adopted the text of the Kyoto Protocol. The – but at the same time maximising efficiency and health situation and/or vaccination shortfalls in al and national action. world’s then leading emitter, the USA (now over- sufficiency, achieving climate-friendly behaviours developing countries will force postponement) is taken by China), refused to ratify. However it came and diets as well as nature-friendly carbon re- billed as ‘the last chance’ to keep the 1.5°C pos- So thank you, Prof. Scoullos, for this timely pub- into force in 2005 mandating modest greenhouse moval through afforestation and land use change sibility open – if total emission reduction com- lication to mobilise Mediterranean citizens and gas emission cuts by 37 industrialised nations while assuring the safe operation of Earth sys- mitments on the table there suffice to deliver the governments and for honouring me with the priv- between 2008 and 2012, subsequently extended tems. -
Climate Change and Human Health: Risks and Responses
Climate change and human health RISKS AND RESPONSES Editors A.J. McMichael The Australian National University, Canberra, Australia D.H. Campbell-Lendrum London School of Hygiene and Tropical Medicine, London, United Kingdom C.F. Corvalán World Health Organization, Geneva, Switzerland K.L. Ebi World Health Organization Regional Office for Europe, European Centre for Environment and Health, Rome, Italy A.K. Githeko Kenya Medical Research Institute, Kisumu, Kenya J.D. Scheraga US Environmental Protection Agency, Washington, DC, USA A. Woodward University of Otago, Wellington, New Zealand WORLD HEALTH ORGANIZATION GENEVA 2003 WHO Library Cataloguing-in-Publication Data Climate change and human health : risks and responses / editors : A. J. McMichael . [et al.] 1.Climate 2.Greenhouse effect 3.Natural disasters 4.Disease transmission 5.Ultraviolet rays—adverse effects 6.Risk assessment I.McMichael, Anthony J. ISBN 92 4 156248 X (NLM classification: WA 30) ©World Health Organization 2003 All rights reserved. Publications of the World Health Organization can be obtained from Marketing and Dis- semination, World Health Organization, 20 Avenue Appia, 1211 Geneva 27, Switzerland (tel: +41 22 791 2476; fax: +41 22 791 4857; email: [email protected]). Requests for permission to reproduce or translate WHO publications—whether for sale or for noncommercial distribution—should be addressed to Publications, at the above address (fax: +41 22 791 4806; email: [email protected]). The designations employed and the presentation of the material in this publication do not imply the expression of any opinion whatsoever on the part of the World Health Organization concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. -
Climate Models and Their Evaluation
8 Climate Models and Their Evaluation Coordinating Lead Authors: David A. Randall (USA), Richard A. Wood (UK) Lead Authors: Sandrine Bony (France), Robert Colman (Australia), Thierry Fichefet (Belgium), John Fyfe (Canada), Vladimir Kattsov (Russian Federation), Andrew Pitman (Australia), Jagadish Shukla (USA), Jayaraman Srinivasan (India), Ronald J. Stouffer (USA), Akimasa Sumi (Japan), Karl E. Taylor (USA) Contributing Authors: K. AchutaRao (USA), R. Allan (UK), A. Berger (Belgium), H. Blatter (Switzerland), C. Bonfi ls (USA, France), A. Boone (France, USA), C. Bretherton (USA), A. Broccoli (USA), V. Brovkin (Germany, Russian Federation), W. Cai (Australia), M. Claussen (Germany), P. Dirmeyer (USA), C. Doutriaux (USA, France), H. Drange (Norway), J.-L. Dufresne (France), S. Emori (Japan), P. Forster (UK), A. Frei (USA), A. Ganopolski (Germany), P. Gent (USA), P. Gleckler (USA), H. Goosse (Belgium), R. Graham (UK), J.M. Gregory (UK), R. Gudgel (USA), A. Hall (USA), S. Hallegatte (USA, France), H. Hasumi (Japan), A. Henderson-Sellers (Switzerland), H. Hendon (Australia), K. Hodges (UK), M. Holland (USA), A.A.M. Holtslag (Netherlands), E. Hunke (USA), P. Huybrechts (Belgium), W. Ingram (UK), F. Joos (Switzerland), B. Kirtman (USA), S. Klein (USA), R. Koster (USA), P. Kushner (Canada), J. Lanzante (USA), M. Latif (Germany), N.-C. Lau (USA), M. Meinshausen (Germany), A. Monahan (Canada), J.M. Murphy (UK), T. Osborn (UK), T. Pavlova (Russian Federationi), V. Petoukhov (Germany), T. Phillips (USA), S. Power (Australia), S. Rahmstorf (Germany), S.C.B. Raper (UK), H. Renssen (Netherlands), D. Rind (USA), M. Roberts (UK), A. Rosati (USA), C. Schär (Switzerland), A. Schmittner (USA, Germany), J. Scinocca (Canada), D. Seidov (USA), A.G. -
Lasting Coastal Hazards from Past Greenhouse Gas Emissions COMMENTARY Tony E
COMMENTARY Lasting coastal hazards from past greenhouse gas emissions COMMENTARY Tony E. Wonga,1 The emission of greenhouse gases into Earth’satmo- 100% sphereisaby-productofmodernmarvelssuchasthe Extremely likely by 2073−2138 production of vast amounts of energy, heating and 80% cooling inhospitable environments to be amenable to human existence, and traveling great distances 60% Likely by 2064−2105 faster than our saddle-sore ancestors ever dreamed possible. However, these luxuries come at a price: 40% climate changes in the form of severe droughts, ex- Probability treme precipitation and temperatures, increased fre- 20% quency of flooding in coastal cities, global warming, RCP2.6 and sea-level rise (1, 2). Rising seas pose a severe risk RCP8.5 0% to coastal areas across the globe, with billions of 2020 2040 2060 2080 2100 2120 2140 US dollars in assets at risk and about 10% of the ’ Year when 50-cm sea-level rise world s population living within 10 m of sea level threshold is exceeded (3–5). The price of our emissions is not felt immedi- ately throughout the entire climate system, however, Fig. 1. Cumulative probability of exceeding 50 cm of sea-level rise by year (relative to the global mean sea because processes such as ice sheet melt and the level from 1986 to 2005). The yellow box denotes the expansion of warming ocean water act over the range of years after which exceedance is likely [≥66% course of centuries. Thus, even if all greenhouse probability (12)], where the left boundary follows a gas emissions immediately ceased, our past emis- business-as-usual emissions scenario (RCP8.5, red line) sions have already “locked in” some amount of con- and the right boundary follows a low-emissions scenario (RCP2.6, blue line). -
Anthropocene
Anthropocene The Anthropocene is a proposed geologic epoch that redescribes humanity as a significant or even dominant geophysical force. The concept has had an uneven global history from the 1960s (apparently, it was used by Russian scientists from then onwards). The current definition of the Anthropocene refers to the one proposed by Eugene F. Stoermer in the 1980s and then popularised by Paul Crutzen. At present, stratigraphers are evaluating the proposal, which was submitted to their society in 2008. There is currently no definite proposed start date – suggestions include the beginnings of human agriculture, the conquest of the Americas, the industrial revolution and the nuclear bomb explosions and tests. Debate around the Anthropocene continues to be globally uneven, with discourse primarily taking place in developed countries. Achille Mbembe, for instance, has noted that ‘[t]his kind of rethinking, to be sure, has been under way for some time now. The problem is that we seem to have entirely avoided it in Africa in spite of the existence of a rich archive in this regard’ (2015). Especially in the anglophone sphere, the image of humanity as a geophysical force has made a drastic impact on popular culture, giving rise to a flood of Anthropocene and geology themed art and design exhibitions, music videos, radio shows and written publications. At the same time, the Anthropocene has been identified as a geophysical marker of global inequality due to its connections with imperialism, colonialism and capitalism. The biggest geophysical impact –in terms of greenhouse emissions, biodiversity loss, water use, waste production, toxin/radiation production and land clearance etc – is currently made by the so-called developed world. -
Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future
Sea-Level Rise for the Coasts of California, Oregon, and Washington: Past, Present, and Future As more and more states are incorporating projections of sea-level rise into coastal planning efforts, the states of California, Oregon, and Washington asked the National Research Council to project sea-level rise along their coasts for the years 2030, 2050, and 2100, taking into account the many factors that affect sea-level rise on a local scale. The projections show a sharp distinction at Cape Mendocino in northern California. South of that point, sea-level rise is expected to be very close to global projections; north of that point, sea-level rise is projected to be less than global projections because seismic strain is pushing the land upward. ny significant sea-level In compliance with a rise will pose enor- 2008 executive order, mous risks to the California state agencies have A been incorporating projec- valuable infrastructure, devel- opment, and wetlands that line tions of sea-level rise into much of the 1,600 mile shore- their coastal planning. This line of California, Oregon, and study provides the first Washington. For example, in comprehensive regional San Francisco Bay, two inter- projections of the changes in national airports, the ports of sea level expected in San Francisco and Oakland, a California, Oregon, and naval air station, freeways, Washington. housing developments, and sports stadiums have been Global Sea-Level Rise built on fill that raised the land Following a few thousand level only a few feet above the years of relative stability, highest tides. The San Francisco International Airport (center) global sea level has been Sea-level change is linked and surrounding areas will begin to flood with as rising since the late 19th or to changes in the Earth’s little as 40 cm (16 inches) of sea-level rise, a early 20th century, when climate. -
Chapter 3. Modelling the Climate System
Introduction to climate dynamics and climate modelling - http://www.climate.be/textbook Chapter 3. Modelling the climate system 3.1 Introduction 3.1.1 What is a climate model ? In general terms, a climate model could be defined as a mathematical representation of the climate system based on physical, biological and chemical principles (Fig. 3.1). The equations derived from these laws are so complex that they must be solved numerically. As a consequence, climate models provide a solution which is discrete in space and time, meaning that the results obtained represent averages over regions, whose size depends on model resolution, and for specific times. For instance, some models provide only globally or zonally averaged values while others have a numerical grid whose spatial resolution could be less than 100 km. The time step could be between minutes and several years, depending on the process studied. Even for models with the highest resolution, the numerical grid is still much too coarse to represent small scale processes such as turbulence in the atmospheric and oceanic boundary layers, the interactions of the circulation with small scale topography features, thunderstorms, cloud micro-physics processes, etc. Furthermore, many processes are still not sufficiently well-known to include their detailed behaviour in models. As a consequence, parameterisations have to be designed, based on empirical evidence and/or on theoretical arguments, to account for the large-scale influence of these processes not included explicitly. Because these parameterisations reproduce only the first order effects and are usually not valid for all possible conditions, they are often a large source of considerable uncertainty in models. -
Interactions Between Changing Climate and Biodiversity: Shaping Humanity's Future
COMMENTARY Interactions between changing climate and biodiversity: Shaping humanity’s future COMMENTARY F. Stuart Chapin IIIa,1 and Sandra Dı´azb,c Scientists have known for more than a century about Harrison et al. (9) note that the climate−diversity potential human impacts on climate (1). In the last 30 y, relationship they document is consistent with a cli- estimates of these impacts have been confirmed and matic tolerance model in which the least drought- refined through increasingly precise climate assess- tolerant species are the first to be lost as climate ments (2). Other global-scale human impacts, including dries. According to this model, drought acts as a filter land use change, overharvesting, air and water pollu- that removes more-mesic–adapted species. Since the tion, and increased disease risk from antibiotic resis- end of the Eocene, about 37 million years ago, Cal- tance, have risen to critical levels, seriously jeopardizing ifornia’s ancient warm-temperate lineages, such as the prospects that future generations can thrive (3–5). redwoods, have retreated into more-mesic habitats, as Earth has entered a stage characterized by human more-drought–adapted lineages like oaks and madrone domination of critical Earth system processes (6–8). spread through California. Perhaps this history of Although the basic trajectories of these changes are declining mesic lineages will repeat itself, if Cal- well known, many of the likely consequences are ifornia’s climate continues to dry over the long term. shrouded in uncertainty because of poorly understood The Harrison study (9) documents several dimen- interactions among these drivers of change and there- sions of diversity that decline with drought. -
The Parallels Between the End-Permian Mass Extinction And
Drawing Connections: The Parallels Between the End-Permian Mass Extinction and Current Climate Change An undergraduate of East Tennessee State University explains that humans’ current effects on the biosphere are disturbingly similar to the circumstances that caused the worst mass extinction in biologic history. By: Amber Rookstool 6 December 2016 About the Author: Amber Rookstool is an undergraduate student at East Tennessee State University. She is currently an English major and dreams of becoming an author and high school English Teacher. She hopes to publish her first book by the time she is 26 years old. Table of Contents Introduction .................................................................................................................................1 Brief Geologic Timeline ...........................................................................................................2 The Anthropocene ......................................................................................................................3 Biodiversity Crisis ....................................................................................................................3 Habitat Loss .........................................................................................................................3 Invasive Species ..................................................................................................................4 Overexploitation ...................................................................................................................4 -
Causes of Sea Level Rise
FACT SHEET Causes of Sea OUR COASTAL COMMUNITIES AT RISK Level Rise What the Science Tells Us HIGHLIGHTS From the rocky shoreline of Maine to the busy trading port of New Orleans, from Roughly a third of the nation’s population historic Golden Gate Park in San Francisco to the golden sands of Miami Beach, lives in coastal counties. Several million our coasts are an integral part of American life. Where the sea meets land sit some of our most densely populated cities, most popular tourist destinations, bountiful of those live at elevations that could be fisheries, unique natural landscapes, strategic military bases, financial centers, and flooded by rising seas this century, scientific beaches and boardwalks where memories are created. Yet many of these iconic projections show. These cities and towns— places face a growing risk from sea level rise. home to tourist destinations, fisheries, Global sea level is rising—and at an accelerating rate—largely in response to natural landscapes, military bases, financial global warming. The global average rise has been about eight inches since the centers, and beaches and boardwalks— Industrial Revolution. However, many U.S. cities have seen much higher increases in sea level (NOAA 2012a; NOAA 2012b). Portions of the East and Gulf coasts face a growing risk from sea level rise. have faced some of the world’s fastest rates of sea level rise (NOAA 2012b). These trends have contributed to loss of life, billions of dollars in damage to coastal The choices we make today are critical property and infrastructure, massive taxpayer funding for recovery and rebuild- to protecting coastal communities. -
Chapter 1 Ozone and Climate
1 Ozone and Climate: A Review of Interconnections Coordinating Lead Authors John Pyle (UK), Theodore Shepherd (Canada) Lead Authors Gregory Bodeker (New Zealand), Pablo Canziani (Argentina), Martin Dameris (Germany), Piers Forster (UK), Aleksandr Gruzdev (Russia), Rolf Müller (Germany), Nzioka John Muthama (Kenya), Giovanni Pitari (Italy), William Randel (USA) Contributing Authors Vitali Fioletov (Canada), Jens-Uwe Grooß (Germany), Stephen Montzka (USA), Paul Newman (USA), Larry Thomason (USA), Guus Velders (The Netherlands) Review Editors Mack McFarland (USA) IPCC Boek (dik).indb 83 15-08-2005 10:52:13 84 IPCC/TEAP Special Report: Safeguarding the Ozone Layer and the Global Climate System Contents EXECUTIVE SUMMARY 85 1.4 Past and future stratospheric ozone changes (attribution and prediction) 110 1.1 Introduction 87 1.4.1 Current understanding of past ozone 1.1.1 Purpose and scope of this chapter 87 changes 110 1.1.2 Ozone in the atmosphere and its role in 1.4.2 The Montreal Protocol, future ozone climate 87 changes and their links to climate 117 1.1.3 Chapter outline 93 1.5 Climate change from ODSs, their substitutes 1.2 Observed changes in the stratosphere 93 and ozone depletion 120 1.2.1 Observed changes in stratospheric ozone 93 1.5.1 Radiative forcing and climate sensitivity 120 1.2.2 Observed changes in ODSs 96 1.5.2 Direct radiative forcing of ODSs and their 1.2.3 Observed changes in stratospheric aerosols, substitutes 121 water vapour, methane and nitrous oxide 96 1.5.3 Indirect radiative forcing of ODSs 123 1.2.4 Observed temperature -
Project Descriptions 2020
Project description / 2020 Health, Risk and Climate Change: Understanding Links Between Exposure, Hazards and Vulnerability Across Spatial and Temporal Scales (HERCULES) Climate related health risks are not yet thoroughly understood. We know that climate change related health risks will be distributed unevenly, with some population groups being more likely to suffer the adverse consequences. Urban populations, especially in socially and economically disadvantaged areas, are likely to be particularly vulnerable to the unfavourable effects of climate change due to already existing exposure to for example, air pollutants and social stressors. What are the specific socio-environmental preconditions that make citizen groups in disadvantaged areas vulnerable to climate change? What are these preconditions, and how are they spatially distributed in cities? What type of actions ought to be taken in order to improve the adaptive capacity and resilience of Finnish cities under climate change? While adaptation within cities has been advancing, there is little knowledge of how adaptation is being implemented and how effective it is. As impacts of climate change are projected to worsen over time, the current adaptation measures may become insufficient, or inappropriate. HERCULES begins from the standpoint that climate change directly influences on individuals’ well-being and health, but that this often happens through long-term, complex, and often concealed processes, including broader trends of urban development. We shall examine how the spatial pattern and intensity of health-relevant climatic hazards and other environmental exposures have changed since the 1980s, and how these will change during the coming decades. For this, we shall use extensive high-resolution data on climate and land-use, and sophisticated modelling.