The Arctic Ozone Layer
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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. -
Ozone Layer Depletion (PDF)
United States Air and Radiation EPA 430-F-10-027 Environmental Protection 6205J August 2010 Agency www.epa.gov/ozone/strathome.html Ozone Layer Depletion The stratospheric ozone layer forms a thin shield in the upper atmosphere, protecting life on Earth from the sun’s ultraviolet (UV) rays. It has been called the Earth’s sunscreen. In the 1980s, scientists found evidence that the ozone layer was being depleted. Depletion of the ozone layer results in increased UV radiation reaching the Earth’s surface, which in turn leads to a greater chance of overexposure to UV radiation and the related health effects of skin cancer, cataracts, and immune suppression. This fact sheet explains the importance of protecting the stratospheric ozone layer. What is Stratospheric Ozone? Ozone is a naturally-occurring gas that can be good or bad for your health and the environment depending on its location in the atmosphere. In the layer near the Earth’s surface—the troposphere— ground-level or “bad” ozone is an air pollutant that is a key ingredient of urban smog. But higher up, in the stratosphere, “good” ozone protects life on Earth by absorbing some of the sun’s UV rays. An easy way to remember this is the phrase “good up high, bad nearby.” Ozone Layer Depletion Compounds that contain chlorine and bromine molecules, such as methyl chloroform, halons, and chlorofluorocarbons (CFCs), are stable and have atmospheric lifetimes long enough to be transported by winds into Ozone “up high” in the stratosphere protects the Earth, while ozone close to the Earth’s surface is harmful. -
Oregon State University Insert PDF 480 K
ARCTIC Arctic Research Consortium of the United States Member Institution Winter 2004/2005, Volume 11 Number 2 Arctic Research at Oregon State University land grant university, Oregon State Geosciences A University was designated as Oregon’s state-assisted agricultural college in 1868. Polar Ice Cores Sea grant and space grant designation came Ed Brook (Geosciences) applies geochemical techniques to diverse problems in late Quater- later, making OSU one of only six universi- nary paleoclimatology; several of his projects have arctic components. NSF-supported work ties to have all three titles. OSU currently focused on the relative timing of millennial-scale abrupt climate change in Greenland and enrolls 15,599 undergraduate and 3,380 Antarctica uses atmospheric methane and the isotopic composition of oxygen as correlation graduate students in more than 200 under- tools to place climate records from the Siple Dome (west Antarctica) and GISP2 (Green- graduate and 80 graduate degree programs. land) ice cores on a precise common chronology for the period from 9–57 ka. The onset With collaborative connections across of major millennial warming events in Siple Dome precedes major abrupt warmings in the globe, OSU researchers contribute to Greenland, and the pattern of millennial change at Siple Dome is broadly similar, though arctic research from disciplines housed in not identical, to that previously observed for the Byrd ice core (also in west Antarctica). a variety of colleges. The College of Oce- The addition of Siple Dome to the database of well-dated Antarctic paleoclimate records anic and Atmospheric Sciences (COAS) supports the case for a regionally consistent pattern of millennial-scale climate change in has several researchers working on arctic Antarctica during the last ice age and glacial-interglacial transition. -
Arctic Climate Change Implications for U.S
Arctic Climate Change Implications for U.S. National Security Perspective - Laura Leddy September 2020 i BOARD OF DIRECTORS The Honorable Gary Hart, Chairman Emeritus Scott Gilbert Senator Hart served the State of Colorado in the U.S. Senate Scott Gilbert is a Partner of Gilbert LLP and Managing and was a member of the Committee on Armed Services Director of Reneo LLC. during his tenure. Vice Admiral Lee Gunn, USN (Ret.) Governor Christine Todd Whitman, Chairperson Vice Admiral Gunn is Vice Chairman of the CNA Military Christine Todd Whitman is the President of the Whitman Advisory Board, Former Inspector General of the Department Strategy Group, a consulting firm that specializes in energy of the Navy, and Former President of the Institute of Public and environmental issues. Research at the CNA Corporation. The Honorable Chuck Hagel Brigadier General Stephen A. Cheney, USMC (Ret.), Chuck Hagel served as the 24th U.S. Secretary of Defense and President of ASP served two terms in the United States Senate (1997-2009). Hagel Brigadier General Cheney is the President of ASP. was a senior member of the Senate Foreign Relations; Banking, Housing and Urban Affairs; and Intelligence Committees. Matthew Bergman Lieutenant General Claudia Kennedy, USA (Ret.) Matthew Bergman is an attorney, philanthropist and Lieutenant General Kennedy was the first woman entrepreneur based in Seattle. He serves as a Trustee of Reed to achieve the rank of three-star general in the United States College on the Board of Visitors of Lewis & Clark Law Army. School. Ambassador Jeffrey Bleich The Honorable John F. Kerry The Hon. -
Global Environmental Issues and Its Remedies
International Journal of Sustainable Energy and Environment Vol. 1, No. 8, September 2013, PP: 120 - 126, ISSN: 2327- 0330 (Online) Available online at www.ijsee.com Research article Global Environmental Issues and its Remedies Dr. MD. Zulfequar Ahmad Khan* Address Present. Permanent Address for Correspondence *Dr. Md Zulfequar Ahmad Khan 21-B, Lane No 3, Associate Professor Jamia Nagar, Zakir Nagar, Department of Geography & Environmental Studies New Delhi-110025 Arba Minch University INDIA Arba Minch, Ethiopia. Mobile No.: +919718502867 Mobile No: +251 923934234 E-mail: [email protected] _____________________________________________________________________________________________ Abstract To the surprise of many out-spoken environmentalists, it, in fact, turns out mankind and technology actually aren’t the only significant causes of global environmental problems. However, before we start to get too comfortable and confidently assume that we as human beings are officially “off the hook,” the fact remains that several “man-made” causes play a significant role in our current, global problems trend. Many human actions affect what people value. One way in which the actions that cause global change are different from most of these is that the effects take decades to centuries to be realized. This fact causes many concerned people to consider taking action now to protect the values of those who might be affected by global environmental change in years to come. But because of uncertainty about how global environmental systems work, and because the people affected will probably live in circumstances very much different from those of today and may have different values, it is hard to know how present-day actions will affect them. -
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 -
Ozone: Good up High, Bad Nearby
actions you can take High-Altitude “Good” Ozone Ground-Level “Bad” Ozone •Protect yourself against sunburn. When the UV Index is •Check the air quality forecast in your area. At times when the Air “high” or “very high”: Limit outdoor activities between 10 Quality Index (AQI) is forecast to be unhealthy, limit physical exertion am and 4 pm, when the sun is most intense. Twenty minutes outdoors. In many places, ozone peaks in mid-afternoon to early before going outside, liberally apply a broad-spectrum evening. Change the time of day of strenuous outdoor activity to avoid sunscreen with a Sun Protection Factor (SPF) of at least 15. these hours, or reduce the intensity of the activity. For AQI forecasts, Reapply every two hours or after swimming or sweating. For check your local media reports or visit: www.epa.gov/airnow UV Index forecasts, check local media reports or visit: www.epa.gov/sunwise/uvindex.html •Help your local electric utilities reduce ozone air pollution by conserving energy at home and the office. Consider setting your •Use approved refrigerants in air conditioning and thermostat a little higher in the summer. Participate in your local refrigeration equipment. Make sure technicians that work on utilities’ load-sharing and energy conservation programs. your car or home air conditioners or refrigerator are certified to recover the refrigerant. Repair leaky air conditioning units •Reduce air pollution from cars, trucks, gas-powered lawn and garden before refilling them. equipment, boats and other engines by keeping equipment properly tuned and maintained. During the summer, fill your gas tank during the cooler evening hours and be careful not to spill gasoline. -
Environmental Effects of Ozone Depletion and Its Interactions with Climate Change: 2010 Assessment
University of Wollongong Research Online Faculty of Science - Papers (Archive) Faculty of Science, Medicine and Health 2010 Environmental Effects of Ozone Depletion and its Interactions with Climate Change: 2010 Assessment Sharon A. Robinson University of Wollongong, [email protected] Stephen R. Wilson University of Wollongong, [email protected] Follow this and additional works at: https://ro.uow.edu.au/scipapers Part of the Life Sciences Commons, Physical Sciences and Mathematics Commons, and the Social and Behavioral Sciences Commons Recommended Citation Robinson, Sharon A. and Wilson, Stephen R.: Environmental Effects of Ozone Depletion and its Interactions with Climate Change: 2010 Assessment 2010. https://ro.uow.edu.au/scipapers/456 Research Online is the open access institutional repository for the University of Wollongong. For further information contact the UOW Library: [email protected] Environmental Effects of Ozone Depletion and its Interactions with Climate Change: 2010 Assessment Abstract This quadrennial Assessment was prepared by the Environmental Effects Assessment Panel (EEAP) for the Parties to the Montreal Protocol. The Assessment reports on key findings on environment and health since the last full Assessment of 2006, paying attention to the interactions between ozone depletion and climate change. Simultaneous publication of the Assessment in the scientific literature aims to inform the scientific community how their data, modeling and interpretations are playing a role in information dissemination to the Parties -
Arctic Policy &
Arctic Policy & Law References to Selected Documents Edited by Wolfgang E. Burhenne Prepared by Jennifer Kelleher and Aaron Laur Published by the International Council of Environmental Law – toward sustainable development – (ICEL) for the Arctic Task Force of the IUCN Commission on Environmental Law (IUCN-CEL) Arctic Policy & Law References to Selected Documents Edited by Wolfgang E. Burhenne Prepared by Jennifer Kelleher and Aaron Laur Published by The International Council of Environmental Law – toward sustainable development – (ICEL) for the Arctic Task Force of the IUCN Commission on Environmental Law The designation of geographical entities in this book, and the presentation of material, do not imply the expression of any opinion whatsoever on the part of ICEL or the Arctic Task Force of the IUCN Commission on Environmental Law concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers and boundaries. The views expressed in this publication do not necessarily reflect those of ICEL or the Arctic Task Force. The preparation of Arctic Policy & Law: References to Selected Documents was a project of ICEL with the support of the Elizabeth Haub Foundations (Germany, USA, Canada). Published by: International Council of Environmental Law (ICEL), Bonn, Germany Copyright: © 2011 International Council of Environmental Law (ICEL) Reproduction of this publication for educational or other non- commercial purposes is authorized without prior permission from the copyright holder provided the source is fully acknowledged. Reproduction for resale or other commercial purposes is prohibited without the prior written permission of the copyright holder. Citation: International Council of Environmental Law (ICEL) (2011). -
Effectiveness of Houseplants in Reducing the Indoor Air Pollutant
as a result of increased input of the Effectiveness of Houseplants in Reducing precursors of ozone into the atmos- the Indoor Air Pollutant Ozone phere (Mustafa, 1990). Automobiles are the principal contributors to sec- ondary tropospheric ozone genera- Heather L. Papinchak1, E. Jay Holcomb2,4, tion (Maroni et al., 1995). Teodora Orendovici Best3, and Dennis R. Decoteau2 Ozone as an indoor air pollutant can be prevalent in homes and offices due to infiltration of outdoor ambient ADDITIONAL INDEX WORDS. mitigation, depletion rates, foliage air indoors (Weschler, 2000). Ozone- emitting equipment such as copy UMMARY Sansevieria trifasciata S . Three common indoor houseplants, snake plant ( ), machines, laser printers, ultraviolet spider plant (Chlorophytum comosum), and golden pothos (Epipremnum aureum), were evaluated for their species effectiveness in reducing ozone concentrations in a lighting, and some electrostatic air simulated indoor environment. Continuously stirred tank reactor (CSTR) chambers purification systems may also contrib- housed within a greenhouse equipped with a charcoal filtration air supply system ute to indoor ozone levels (Maroni were used to simulate an indoor environment in which ozone concentrations could et al., 1995; Weschler, 2000). Ozone be measured and regulated. Ozone was injected into the chambers and when generation from appliances such as concentrations reached 200 ± 5 ppb, the ozone-generating system was turned off photocopiers on average yield 5.2 and ozone concentrations over time (ozone was monitored every 5–6 min in each mgÁh–1 and laser printers on average chamber) were recorded until about <5 ppb were measured in the treatment produce 1.2 mgÁh–1; however, con- chamber. On average, ozone depletion time (time from when the ozone generating centrations could vary based on < system was turned off at 200 ppb to 5 ppb in the chamber) ranged from 38 to equipment maintenance (Black and 120 min per evaluation. -
Air Pollution in Cold Regions - Philip K
COLD REGIONS SCIENCE AND MARINE TECHNOLOGY - Air Pollution in Cold Regions - Philip K. Hopke AIR POLLUTION IN COLD REGIONS Philip K. Hopke Center for Air Resource Engineering and Science, Clarkson University Keywords: air pollution, particulate matter, Arctic Haze, ozone, mercury, depletion events Contents 1. Introduction 2. Arctic Air Pollution 2.1. Particulate Matter 2.1.1. Introduction 2.1.2. Long Term Monitoring Programs 2.1.3. Source-Receptor Relationships 2.1.4. Concentration Trends 2.2. Arctic Photochemistry 3. Antarctic Pollution 4. Conclusions Glossary Bibliography Biographical Sketch Summary This chapter provides an overview of the nature of the constituents in the atmosphere and the changes in concentrations of these constituents that is termed air pollution. The focus will be on the changes in the cold regions of the earth with emphasis on the polar areas, the Arctic and the Antarctic. Although there is limited anthropogenic activity in these areas, there are concentrations of atmospheric constituents that are above those levels that are likely to have been present before the start of the industrial revolution. These changes can be both qualitative and quantitative. The nature of the sources, transport, and chemical processes that lead to the pollution of these regions is described. UNESCO – EOLSS 1. Introduction The atmosphere is a complex chemical system that has evolved through interactions with the lithosphere,SAMPLE hydrosphere and bios phere.CHAPTERS Gases and particles are exchanged between the surfaces of the land and water. There are gaseous and particulate emissions from plants and animals as well as from anthropogenic activities. They undergo complex chemical processing driven primarily by sunlight so that the cold regions of the world present unique circumstances because there are periods with no or so little sunlight as to halt photochemical processing. -
The Ozone Layer Our Global Sunscreen by Mike Carlowicz
The Ozone Layer Our Global Sunscreen By Mike Carlowicz t’s not often that scientists get to conduct experiments that seem like they come out of a A good idea with a science fiction novel or a video game. Yet, that is what some researchers at NASA did a few bad outcome years ago. Atmospheric physicists Paul Newman and Luke Oman built a simulation of the Earth’s The experiments run by Newman and atmosphere and then proceeded to strip away our protective ozone layer. Their computer colleagues were actually extensions of an model reproduced the chemistry and circulation of the air; natural variations in temperatures and experiment that humans have been unwit- winds; and minor changes in the energy received from the sun. Newman and Oman then added tingly running with Earth for nearly a cen- ozone-destroying chemicals to the atmosphere at a rate of 3% more per year—on top of what tury. Humans have been depleting the ozone was already in our 1970s atmosphere. For several months, they ran their model on a supercom- layer with chemical products. puter and reproduced about 80 years of simulated Earth time. They called their experiment “The The unintentional experiment started World Avoided.” in the late 1920s, when Thomas Midgley By the year 2020 in the simulation, 17% of the Earth’s protective ozone layer vanished. Holes Jr. and other industrial chemists began to in the ozone layer formed not just over Antarctica—as they currently do each spring—but over produce chlorofluorocarbons (CFCs), non- the Arctic, too. By 2040, the ultraviolet (UV) index, the measure of the sunburn-causing radiation toxic compounds that improved refrigera- reaching the Earth’s surface, rose as high as 15 on summer days in mid-latitude cities such as tion.