Is Rapid Climate Change in the Arctic a Planetary Emergency? Peter Carter, November 2013 Updated 2019
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Modelling Coupled Oscillations of Volcanic CO2 Emissions and Glacial Cycles
Modelling Coupled Oscillations of Volcanic CO2 Emissions and Glacial Cycles Jonathan M.A. Burley∗1, Peter Huybers2, and Richard F. Katz1 1Department of Earth Sciences, University of Oxford, UK 2Department of Earth and Planetary Sciences, Harvard University, Cambridge, USA October 30, 2017 1 Introduction Following the mid-Pleistocene transition, glacial cycles changed from 40 kyr cycles to longer 80 or 120 kyr cycles[Lisiecki and Raymo, 2005, Elderfield et al., 2012]. The 40 kyr glacial cycles are broadly accepted as being driven by cyclical changes in Earth’s orbital parameters and the consequent insolation changes — Milankovitch cycles. However, Milankovitch forcing does not readily explain the > 40 kyr glacial cycles that occur after the mid-Pleistocene transition. These > 40 kyr cycles therefore require that internal dynamics in the Earth system create a glacial response that is not linearly related to insolation [Tziperman et al., 2006]. Any proposed mechanism to extend glacial cycles’ periods beyond 40 kyrs must give the Earth’s climate system a memory on the order of 10s-of-kyrs, creating either a response that counteracts the 40 kyr Milankovitch forcing (allowing the Earth to ‘skip’ beats in the 40 kyr forcing) or a climate state with sufficient inertia — low climate sensitivity — that it is not af- fected by 40 kyr obliquity forcing [Imbrie and Imbrie, 1980]. The atmosphere/ocean has typical adjustment timescales on the order of 1000 years, thus oceanic theories for glacial cycles rely on other, long-timescale processes (eg. weathering [Toggweiler, 2008]) to trigger arbitrary rules- based switches in the oceanic carbon system at tens-of thousands-of-years intervals. -
Reduced Net Methane Emissions Due to Microbial Methane Oxidation in a Warmer Arctic
LETTERS https://doi.org/10.1038/s41558-020-0734-z Reduced net methane emissions due to microbial methane oxidation in a warmer Arctic Youmi Oh 1, Qianlai Zhuang 1,2,3 ✉ , Licheng Liu1, Lisa R. Welp 1,2, Maggie C. Y. Lau4,9, Tullis C. Onstott4, David Medvigy 5, Lori Bruhwiler6, Edward J. Dlugokencky6, Gustaf Hugelius 7, Ludovica D’Imperio8 and Bo Elberling 8 Methane emissions from organic-rich soils in the Arctic have bacteria (methanotrophs) and the remainder is mostly emitted into been extensively studied due to their potential to increase the atmosphere (Fig. 1a). The methanotrophs in these wet organic the atmospheric methane burden as permafrost thaws1–3. soils may be low-affinity methanotrophs (LAMs) that require However, this methane source might have been overestimated >600 ppm of methane (by moles) for their growth and mainte- without considering high-affinity methanotrophs (HAMs; nance23. But in dry mineral soils, the dominant methanotrophs are methane-oxidizing bacteria) recently identified in Arctic min- high-affinity methanotrophs (HAMs), which can survive and grow 4–7 eral soils . Herein we find that integrating the dynamics of at a level of atmospheric methane abundance ([CH4]atm) of about HAMs and methanogens into a biogeochemistry model8–10 1.8 ppm (Fig. 1b)24. that includes permafrost soil organic carbon dynamics3 leads Quantification of the previously underestimated HAM-driven −1 to the upland methane sink doubling (~5.5 Tg CH4 yr ) north of methane sink is needed to improve our understanding of Arctic 50 °N in simulations from 2000–2016. The increase is equiva- methane budgets. -
Working Towards a Just Peace in the Middle East
KAIROS Policy Briefing Papers are written to help inform public debate on key domestic and foreign policy issues No. 41 April 2015 Hopeful Signs, Alarming Realities on the Road to Climate Justice By John Dillon Ecological Economy Program Coordinator “Climate change for us is a matter of life or death.”1 waiting for the Paris conference to make decisions These stark words were spoken by Rev. Tafue Lu- that, in most cases, will take effect only in 2020. sama, General Secretary of the Tuvalu Christian Church, in September 2014 at an interfaith summit in New York. How prophetic they were in March 2015 when Super Cyclone Pam wreaked havoc on the Pa- cific island state, killing dozens and destroying thou- sands of homes in neighbouring Vanuatu. Rising sea levels and warmer water temperatures have increased the frequency and intensity of tropical storms like this one and Typhoon Haiyan, which struck the Philip- pines in 2013. Yet, although climate change is already devastating the lives of millions of vulnerable people, Rev. Olav Cyclone Pam survivors survey damage in Vanuatu. Tveit, General Secretary of the World Council of Churches, reminds us: “Despite all the negative condi- Hopeful signs include initiatives being undertaken tions, we have the right to hope, not as a passive wait- by some Canadian provinces such as putting a price ing but as an active process towards justice and on carbon emissions and declaring moratoria on hy- peace.”2 This Briefing Paper examines some hopeful draulic fracturing (fracking) to extract shale gas. As signs of progress in the struggle for climate justice, well, a number of civil society groups, such as Cli- despite major obstacles. -
FIRST-ORDER DRAFT IPCC WGII AR5 Chapter 19 Do Not Cite, Quote
FIRST-ORDER DRAFT IPCC WGII AR5 Chapter 19 1 Chapter 19. Emergent Risks and Key Vulnerabilities 2 3 Coordinating Lead Authors 4 Michael Oppenheimer (USA), Maximiliano Campos (Costa Rica) 5 6 Lead Authors 7 Joern Birkmann (Germany), George Luber (USA), Brian O’Neill (USA), Kiyoshi Takahashi (Japan), Rachel Warren 8 (UK) 9 10 Contributing Authors 11 Franz Berkhout (Netherlands), Pauline Dube (Botswana), Wendy Foden (South Africa), Stefan Greiving (Germany), 12 Solomon Hsiang (USA), Klaus Keller (USA), Joan Kleypas (USA), Robert Kopp (USA), Carlos Peres (UK), Jeff 13 Price (UK), Alan Robock (USA), Wolfram Schlenker (USA), Richard Tol (UK) 14 15 Review Editors 16 Mike Brklacich (Canada), Sergey Semenov (Russian Federation) 17 18 Chapter Scientist 19 Solomon Hsiang (USA) 20 21 22 Contents 23 24 Executive Summary 25 26 19.1. Purpose, Scope, and Structure of the Chapter 27 19.1.1. Historical Development of this Chapter 28 19.1.2. The Special Report on Managing the Risks of Extreme Events and Disasters to Advance Climate 29 Change Adaptation (SREX) 30 19.1.3. New Developments in this Chapter 31 32 19.2. Framework for Identifying Key Vulnerabilities, Key Risks, and Emergent Risks 33 19.2.1. Risk and Vulnerability 34 19.2.2. Criteria for Identifying Key Vulnerabilities and Key Risks 35 19.2.2.1. Criteria for Identifying Key Vulnerabilities 36 19.2.2.2. Criteria for Identifying Key Risks 37 19.2.3. Criteria for Identifying Emergent Risks 38 19.2.4. Identifying Key and Emergent Risks under Alternative Development Pathways 39 19.2.5. Assessing Key Vulnerabilities and Emergent Risks 40 41 19.3. -
Forest Conservation and Management in The
Management in a Changing Climate Policy Challenges for Wildlife Abstract: Try as it might, wildlife management cannot make wild living things adapt to climate change. Management can, Mark L. Shaffer however, make adaptation more or less likely. Given that pol- Office of the Science Advisor, icy is a rule set for action, policy will play a critical role in U.S. Fish and Wildlife Service society’s efforts to help wildlife cope with the challenge of cli- mate change. To be effective, policy must provide clear goals and be based on a clear understanding of the problem it seeks to affect. The “National Fish, Wildlife, and Plants Climate Ad- aptation Strategy” provides seven major goals and numerous policy related actions for wildlife management in a period of climate change. The underlying themes of these recommenda- tions and the major challenges to their achievement are identi- fied and discussed. INTRODUCTION As one of the major biome types on Earth, forests are of fundamental importance to wildlife. (Note: the term “wildlife” when used alone is meant as short hand for all species living in an undomesticated state: both plant and animal.) From the standpoint of species diversity, the most diverse terrestrial habitats on Earth are the great tropical rainforests. From the standpoint of sheer stand- ing biomass, the great temperate rainforest of the Pacific Northwest may be unequalled. In terms of charismatic megafauna, which for most people are the face of wild- life, many signature North American species (e.g., deer, bear, elk, wolf, moose, cougar) are principally forest spe- cies. A large fraction of the lands American society has chosen to devote to conservation are forested lands. -
Steering the Climate System: Using Inertia to Lower the Cost of Policy: Comment
Steering the Climate System: Using Inertia to Lower the Cost of Policy: Comment The MIT Faculty has made this article openly available. Please share how this access benefits you. Your story matters. Citation Mattauch, Linus, et al. "Steering the Climate System: Using Inertia to Lower the Cost of Policy: Comment." American Economic Review, 110, 4 (April 2020): 1231-37. As Published http://dx.doi.org/10.1257/aer.20190089 Publisher American Economic Association Version Final published version Citable link https://hdl.handle.net/1721.1/125321 Terms of Use Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. American Economic Review 2020, 110(4): 1231–1237 https://doi.org/10.1257/aer.20190089 Steering the Climate System: Using Inertia to Lower the Cost of Policy: Comment† By Linus Mattauch, H. Damon Matthews, Richard Millar, Armon Rezai, Susan Solomon, and Frank Venmans* Lemoine and Rudik 2017 argues that it is efficient to delay reduc- ing carbon emissions(, due )to supposed inertia in the climate system’s response to emissions. This conclusion rests upon misunderstand- ing the relevant earth system modeling: there is no substantial lag between CO2 emissions and warming. Applying a representation of the earth system that captures the range of responses seen in complex earth system models invalidates the original article’s implications for climate policy. The least-cost policy path that limits warming to 2°C implies that the carbon price starts high and increases at the interest rate. -
ON the RISK of OVERSHOOTING 2°C Paper Presented at Scientific Symposium “Avoiding Dangerous Climate Change”, Metoffice, Exeter, 1-3 February 2005
MEINSHAUSEN – ON THE RISK OF OVERSHOOTING 2°C Paper presented at Scientific Symposium “Avoiding Dangerous Climate Change”, MetOffice, Exeter, 1-3 February 2005 On the Risk of Overshooting 2°C Malte Meinshausen Swiss Federal Institute of Technology (ETH Zurich), Environmental Physics, Department of Environmental Sciences, Rämistrasse 101, CH-8092 Zurich, Switzerland, Email: [email protected] Abstract This article explores different greenhouse gas stabilization levels and their implied risks of overshooting certain temperature targets, such as limiting global mean temperature rise to 2°C above pre-industrial levels. The probabilistic assessment is derived from a compilation of recent estimates of the uncertainties in climate sensitivity, which summarizes the key uncertainties in climate science for long-term temperature projections. The risk of overshooting 2°C equilibrium warming is found to lie between 68% and 99% for stabilization at 550ppm CO2 equivalence. Only at levels around 400ppm CO2 equivalence are the risks of overshooting low enough so that the achievement of a 2°C target can be termed “likely”. Based on characteristics of 54 IPCC SRES and post-SRES scenarios, multi-gas emission pathways are presented that lead to stabilization at 550, 450 and 400ppm CO2eq in order to assess the implications for global emission reductions. Sensitivity studies on delayed global action show that the next 5 to 15 years might determine whether the risk of overshooting 2°C can be limited to a reasonable range. 1. Introduction For these reasons, this study focuses on an 2 analysis of the risk of overshooting global mean In 1996, the European Council adopted a temperature levels of 2°C above pre-industrial climate target that reads “[…] the Council believes levels. -
Climate Change
duurzameMOS scholen straffe scholen Climate Change Causes, effects and solutions DEPARTEMENT OMGEVING mosvlaanderen.be REFERENCES IPCC reports are the main sources used to write this mind map and the accompanying text. The different IPCC reports contain an abundance of climate information. You can download them for free on the official IPCC website: www.ipcc.ch/reports. (Currently) the most important ones are: • IPCC. (2013). Climate change 2013: The physical science basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. [Stocker, T.F., et al. (Eds.)] Cambridge: Cambridge University Press. • IPCC. (2014). Climate change 2014: Mitigation of climate change. Contribution of Working Group III to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change. [Edenhofer, O., et al. (Eds.)] Cambridge: Cambridge University Press. • IPCC. (2018). Global warming of 1.5°C. An IPCC Special Report on the impacts of global warming of 1.5°C above pre-industrial levels and related global greenhouse gas emission pathways, in the context of strengthening the global response to the threat of climate change, sustainable development, and efforts to eradicate poverty. [V. Masson-Delmotte, et al. (eds.)]. In Press. • IPCC. (2019). IPCC Special Report on Climate Change, Desertification, Land Degradation, Sustainable Land Management, Food Security, and Greenhouse gas fluxes in Terrestrial Ecosystems. [Almut Arneth, et al. (eds.)]. In Press. • IPCC. (2019). IPCC Special Report on the Ocean and Cryosphere in a Changing Climate. [H.- O. Pörtner, et al. (eds.)]. In Press. The IPCC has a website specifically for teachers: www.oce.global/en/resources/ipcc-summaries-teachers This is where you will find a summary of the IPCC report for teachers: www.ipcc.ch/site/assets/uploads/sites/2/2018/12/ST1.5_OCE_LR.pdf Other sources include: • EUROPEAN COMMISSION. -
IPCC Special Report "Global Warming of 1.5°C"
IPCC SPECIAL REPORT GLOBAL WARMING OF 1.5°C SUMMARY FOR TEACHERS Coordinator Lydie Lescarmontier (OCE, France) Authors (in alphabetical order) Eric Guilyardi (IPSL, France), Lydie Lescarmontier (OCE, France), Robin Matthews (IPCC Working Group I Technical Support Unit, France), Sakina Pen Point (OCE, France), Anwar Bhai Rumjaun (Mauritius Institute of Education, Mauritius), Jenny Schlüpmann (Freie Universität Berlin, Germany), David Wilgenbus (OCE, France) Copy editors (in alphabetical order) Badin Borde (Siemens Stiftung, Germany), Raphaëlle Kounkou-Arnaud (Météo-France, France), Maria A. Martin (Potsdam Institute for Climate Impact Research, Germany), Christine Niewöhner (Siemens Stiftung, Germany), Vincent Viguié (CIRED, France) Acknowledgements Technical Support Unit of IPCC Working Group I for provision of background information Date of Publication December 2018 Photos John Salvino (cover) This work (excluding photos) has Patrick Hendry (page 8) been published under the follow- Bill Wegener (page 11 & 23) ing Creative Commons licence. VanveenJF (page 13) It is free to share, use and adapt NASA (page 16) with no commercial use. Juha Lakaniemi (page 17) John Westrock (page 21) Art work Mareva Sacoun ([email protected]). Summary Introduction 5 A. Understanding global warming 7 B. Climate change impacts at 1.5°C and 2°C 14 C. How can warming be limited to 1.5°C ? 18 D. Addressing climate change in the context of sustainable development 20 Glossary 22 Resources 23 “ Each degree matters, each year matters, and each decision matters : not acting today is adding to the burden of the next generations [...]. Limiting global warming to 1.5°C is not impossible but requires strong and immediate policies. -
Stolerov Arctic Meth
Critical Review pubs.acs.org/est Review of Methane Mitigation Technologies with Application to Rapid Release of Methane from the Arctic Joshuah K. Stolaroff,* Subarna Bhattacharyya, Clara A. Smith, William L. Bourcier, Philip J. Cameron-Smith, and Roger D. Aines Lawrence Livermore National Laboratory, Livermore, California, United States *S Supporting Information ABSTRACT: Methane is the most important greenhouse gas after carbon dioxide, with particular influence on near-term climate change. It poses increasing risk in the future from both direct anthropogenic sources and potential rapid release from the Arctic. A range of mitigation (emissions control) technologies have been developed for anthropogenic sources that can be developed for further application, including to Arctic sources. Significant gaps in understanding remain of the mechanisms, magnitude, and likelihood of rapid methane release from the Arctic. Methane may be released by several pathways, including lakes, wetlands, and oceans, and may be either uniform over large areas or concentrated in patches. Across Arctic sources, bubbles originating in the sediment are the most important mechanism for methane to reach the atmosphere. Most known technologies operate on confined gas streams of 0.1% methane or more, and may be applicable to limited Arctic sources where methane is concentrated in pockets. However, some mitigation strategies developed for rice paddies and agricultural soils are promising for Arctic wetlands and thawing permafrost. Other mitigation strategies specific to the Arctic have been proposed but have yet to be studied. Overall, we identify four avenues of research and development that can serve the dual purposes of addressing current methane sources and potential Arctic sources: (1) methane release detection and quantification, (2) mitigation units for small and remote methane streams, (3) mitigation methods for dilute (<1000 ppm) methane streams, and (4) understanding methanotroph and methanogen ecology. -
Toward a Responsible Solar Geoengineeri...Ram
1/12/2018 Toward a Responsible Solar Geoengineering Research Program | Issues in Science and Technology Toward a Responsible Solar Geoengineering Research Program by David W. Keith The seriousness of the risks posed by climate change demands that we examine all possible means of response, but how we do so makes all the dierence. A combination of greenhouse-gas emission cuts and solar geoengineering could keep temperatures under the 1.5-degree aspirational target of the recent Paris Agreement. It could make the world cooler at the century’s end than it is today. Emissions cuts alone cannot achieve either objective with high condence. The climate’s inertia along with uncertain feedbacks such as loss of permafrost carbon mean there is a small but signicant chance that the world will continue to warm for more than a century after emissions stop. Solar geoengineering is the process by which humans might deliberately reduce the eect of heat- trapping greenhouses gases, particularly carbon dioxide, by reecting a small fraction of sunlight back to space. The most plausible solar geoengineering technology appears to be the addition of aerosols (ne droplets or powder) to the stratosphere, where they would scatter some sunlight back to space, thus cooling the planet by reducing the amount of heat that enters the atmosphere. Solar geoengineering could also limit global warming’s predicted side eects such as sea level rise and changes in precipitation and other weather patterns. Because these changes would have their most powerful impact on the world’s most vulnerable people, who lack the resources to move or adapt, one can make a strong ethical case for research to explore the technology. -
Climate Change Fact Sheet Series: KS4 & a 51 ACE Information Programme Aric Simple Climate Model
ACE Information Programme aric Introduction The word "detection" by climate scientists has been used to refer to the identification of the significant change in climate during the twentieth century and its "attribution" to the enhanced greenhouse effect due to man-made greenhouse gas emissions. Most reviews have noted that the global average temperature change over the past 100 years is consistent with the enhanced greenhouse effect theory. This fact sheet reviews the evidence for a causal link between the man-made enhancement of the greenhouse effect and the observed global warming. The difficulty in “greenhouse detection and attribution” arises because there are numerous other causes of climatic variability, and some of these may be operating on time scales (10 to 100 years) comparable to that of the enhanced greenhouse effect. In addition, the inherent variability (random fluctuations) of the climate system can produce warming or cooling trends of up to 0.3oC per century. Greenhouse Modelling versus Observation Global average temperature has increased by around 0.4 to 0.8oC over the past 100 years. At the same time, greenhouse gas concentrations, and atmospheric aerosols emissions, have increased substantially. To assess whether the two are associated requires the use of computer model simulations of the likely climatic effects of the changing atmospheric composition, and the comparison of the results with observations. The diagram below compares the observational global temperature record (solid line) with different model scenarios (dashed lines) from a Global Climate Change Fact Sheet Series: KS4 & A 51 ACE Information Programme aric simple climate model. The different model scenarios represent different possibilities of the sensitivity of the global climate.