The Latest Myths and Facts on Global Warming
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Aerosol Effective Radiative Forcing in the Online Aerosol Coupled CAS
atmosphere Article Aerosol Effective Radiative Forcing in the Online Aerosol Coupled CAS-FGOALS-f3-L Climate Model Hao Wang 1,2,3, Tie Dai 1,2,* , Min Zhao 1,2,3, Daisuke Goto 4, Qing Bao 1, Toshihiko Takemura 5 , Teruyuki Nakajima 4 and Guangyu Shi 1,2,3 1 State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China; [email protected] (H.W.); [email protected] (M.Z.); [email protected] (Q.B.); [email protected] (G.S.) 2 Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters/Key Laboratory of Meteorological Disaster of Ministry of Education, Nanjing University of Information Science and Technology, Nanjing 210044, China 3 College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100029, China 4 National Institute for Environmental Studies, Tsukuba 305-8506, Japan; [email protected] (D.G.); [email protected] (T.N.) 5 Research Institute for Applied Mechanics, Kyushu University, Fukuoka 819-0395, Japan; [email protected] * Correspondence: [email protected]; Tel.: +86-10-8299-5452 Received: 21 September 2020; Accepted: 14 October 2020; Published: 17 October 2020 Abstract: The effective radiative forcing (ERF) of anthropogenic aerosol can be more representative of the eventual climate response than other radiative forcing. We incorporate aerosol–cloud interaction into the Chinese Academy of Sciences Flexible Global Ocean–Atmosphere–Land System (CAS-FGOALS-f3-L) by coupling an existing aerosol module named the Spectral Radiation Transport Model for Aerosol Species (SPRINTARS) and quantified the ERF and its primary components (i.e., effective radiative forcing of aerosol-radiation interactions (ERFari) and aerosol-cloud interactions (ERFaci)) based on the protocol of current Coupled Model Intercomparison Project phase 6 (CMIP6). -
A General Theory of Climate Denial Peter J
A General Theory of Climate Denial Peter J. Jacques A General Theory of Climate Denial • Peter J. Jacques There is now a well-recognized right-wing counter-movement challenging the trend, attribution, impact, and civic implications of orthodox climate change science. Where do the body and spirit of this counter-movement come from? Here I will reºect on some conspicuous questions. First, why have academics, the media, and the counter-movement itself had difªculty naming the counter- movement? Second, why reject the premise of global environmental change at all? Finally, what is the result of the apparent binary choice between the ac- knowledgment of the orthodoxy and its rejection? A General Theory of Denial I will argue that climate denial is an appropriate label consistent with Lang’s “General Theory of Historical Denial.”1 Currently, there is disagreement whether climate “skeptic,” “contrarian,” and “denier” are representative terms.2 I have used the word “skeptic,” but I admit here and elsewhere that it is inappro- priate,3 because the skepticism in environmental skepticism is asymmetrical. As skeptics cast doubt on ecological science, they have an abiding faith in industrial science and technology, free enterprise, and those great institutions of Western Enlightenment.4 Further, skeptics rightfully argue that skepticism is a funda- mental sentiment of rigorous science. Ecological cynicism is then positioned as scientiªc without drawing attention to the asymmetry. Lahsen has successfully used the word “contrarian” to denote the most outspoken leaders of climate rejection, particularly credentialed physicists and climate scientists such as Frederick Seitz, Robert Jastrow, William Nierenberg, Willie Soon, and Sallie Balliunas. -
Richard J. Reed 1922–2008
Richard J. Reed 1922–2008 A Biographical Memoir by John M. Wallace ©2015 National Academy of Sciences. Any opinions expressed in this memoir are those of the author and do not necessarily reflect the views of the National Academy of Sciences. RICHARD JOHN REED June 18, 1922–February 4, 2008 Elected to the NAS, 1978 Richard John Reed, known to his friends as Dick Reed, was trained as a synoptic meteorologist of the “old school.” He derived aesthetic enjoyment from depicting weather patterns and was exhilarated by the competitive aspect of weather prediction. He practiced weather fore- casting when it was still an art and he was good at it. Upon learning of Reed’s death, his long time friend, Richard Goody remarked, “There is a sense in which Dick’s passing marks the end of an era in American meteorology.” Reed also helped to usher in a new era: he was among the leaders in the late-20th-century revolution that trans- formed weather forecasting from an art into a science. Along the way, Reed surveyed, contemplated, and wrote By John M. Wallace about the wonders of the atmosphere: the long range transport of stratospheric ozone; a remarkable quasi-bi- ennial periodicity in stratospheric winds; sudden warmings of the stratospheric polar cap region; atmospheric tides; clear air turbulence; tropical waves and their embedded deep cumulus convection; severe local wind storms; cyclones over the polar regions; rapidly deepening extratropical cyclones; and bogus sightings of flying saucers. Reflecting back on his diverse array of research interests many years later, Reed reflected, “I was like a kid in a candy shop.” Colleagues and former students fondly recall his high energy level, his boundless curiosity, and his expressive and contagious enthusiasm. -
Short- and Long-Term Greenhouse Gas and Radiative Forcing Impacts of Changing Water Management in Asian Rice Paddies
Global Change Biology (2004) 10, 1180–1196, doi: 10.1111/j.1365-2486.2004.00798.x Short- and long-term greenhouse gas and radiative forcing impacts of changing water management in Asian rice paddies STEVE FROLKING*,CHANGSHENGLI*, ROB BRASWELL* andJAN FUGLESTVEDTw *Institute for the Study of Earth, Oceans, & Space, 39 College Road, University of New Hampshire, Durham, NH 03824, USA, wCICERO, Center for International Climate and Environmental Research – Oslo, PO Box 1129, Blindern, 0318 Oslo, Norway Abstract Fertilized rice paddy soils emit methane while flooded, emit nitrous oxide during flooding and draining transitions, and can be a source or sink of carbon dioxide. Changing water management of rice paddies can affect net emissions of all three of these greenhouse gases. We used denitrification–decomposition (DNDC), a process-based biogeochemistry model, to evaluate the annual emissions of CH4,N2O, and CO2 for continuously flooded, single-, double-, and triple-cropped rice (three baseline scenarios), and in further simulations, the change in emissions with changing water management to midseason draining of the paddies, and to alternating crops of midseason drained rice and upland crops (two alternatives for each baseline scenario). We used a set of first- order atmospheric models to track the atmospheric burden of each gas over 500 years. We evaluated the dynamics of the radiative forcing due to the changes in emissions of CH4, N2O, and CO2 (alternative minus baseline), and compared these with standard calculations of CO2-equivalent emissions using global warming potentials (GWPs). All alternative scenarios had lower CH4 emissions and higher N2O emissions than their corresponding baseline cases, and all but one sequestered carbon in the soil more slowly. -
Abstracts Connecting to the Boston University Network
20th Cambridge Workshop: Cool Stars, Stellar Systems, and the Sun July 29 - Aug 3, 2018 Boston / Cambridge, USA Abstracts Connecting to the Boston University Network 1. Select network ”BU Guest (unencrypted)” 2. Once connected, open a web browser and try to navigate to a website. You should be redirected to https://safeconnect.bu.edu:9443 for registration. If the page does not automatically redirect, go to bu.edu to be brought to the login page. 3. Enter the login information: Guest Username: CoolStars20 Password: CoolStars20 Click to accept the conditions then log in. ii Foreword Our story starts on January 31, 1980 when a small group of about 50 astronomers came to- gether, organized by Andrea Dupree, to discuss the results from the new high-energy satel- lites IUE and Einstein. Called “Cool Stars, Stellar Systems, and the Sun,” the meeting empha- sized the solar stellar connection and focused discussion on “several topics … in which the similarity is manifest: the structures of chromospheres and coronae, stellar activity, and the phenomena of mass loss,” according to the preface of the resulting, “Special Report of the Smithsonian Astrophysical Observatory.” We could easily have chosen the same topics for this meeting. Over the summer of 1980, the group met again in Bonas, France and then back in Cambridge in 1981. Nearly 40 years on, I am comfortable saying these workshops have evolved to be the premier conference series for cool star research. Cool Stars has been held largely biennially, alternating between North America and Europe. Over that time, the field of stellar astro- physics has been upended several times, first by results from Hubble, then ROSAT, then Keck and other large aperture ground-based adaptive optics telescopes. -
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 -
The Use of Non-CO2 Multipliers for the Climate Impact of Aviation: the Scientific Basis
Workshop on Aviation and Carbon Markets ICAO Headquarters Montreal, Quebec 18-19 June 2008 The use of non-CO2 multipliers for the climate impact of aviation: The scientific basis by Dr. David W. Fahey Earth System Research Laboratory National Oceanic and Atmospheric Administration Boulder, Colorado USA Introduction Outline Aviation and climate change radiative forcings The multiplier concept and limitations Conclusions & recommendations 1 Introduction Aviation contributes to climate change by increasing atmospheric radiative forcing through the emission of gases and aerosols and changing cloud abundance. Radiative forcing is a change in the balance of solar and terrestrial radiation in Earth’s atmosphere. IPCC, AR4 (2007) 2 1 Aviation and climate change Adapted from Wuebbles et al., 2007 3 Aviation and climate change CO2 Non-CO2 The non-CO2 multiplier is an effort to simplify the accounting of aviation climate forcing from effects other than CO2 accumulation. Adapted from Wuebbles et al., 2007 4 2 Global radiative forcing components (1750 - 2005) * Cooling Warming Aviation represents 3% (range 2 - 8%) of anthropogenic radiative forcing in 2005 (includes all components except induced cloudiness) * 5 Adapted from IPCC, AR4 (2007) Global radiative forcing components (1750 - 2005) Aviation RF components Aviation represents 3% (range 2 - 8%) of anthropogenic radiative forcing in 2005 *(includes all components except induced cloudiness) Adapted from IPCC, AR4 (2007) 6 3 Aviation radiative forcing components (1750 - 2005) Cooling Warming Aviation radiative forcing components have been quantified with best estimates except for induced cirrus cloudiness which includes aerosol cloud effects. Radiative forcing is a backward-looking metric that integrates over previous aircraft operations (i.e., 1750-2005) and hence is not a suitable metric for future aviation. -
Impacts of Biofuels on Climate Change, Water Use, and Land Use MARK A
PUBLIC INTEREST REPORT SUMMER 2011 Impacts of Biofuels on Climate Change, Water Use, and Land Use MARK A. DELUCCHI * INTRODUCTION Governments worldwide are promoting the and land use – because per unit of energy development of biofuels, such as ethanol from produced, biofuels require orders of magnitude corn, biodiesel from soybeans, and ethanol from more land and water than do petroleum wood or grass, in order to reduce dependency transportation fuels – and these impacts should on oil imported from politically unstable be weighed in an overall assessment of the costs regions of the world, spur agricultural and benefits of policies that promote biofuels. development, and reduce the climate impact of fossil fuel combustion. Biofuels have been At the start of each major section, I first discuss promoted as a way to mitigate the climate- the overall metric by which impacts typically are change impacts of energy use because the measured. is overall metric is important carbon in a biofuel comes from the atmosphere, because many analysts use it is a basis for which means that the combustion of a biofuel evaluating and comparing the impacts of biofuels; returns to the atmosphere the amount of hence, the overall metric should be as broad as carbon dioxide (CO2) that was removed by the possible yet still represent what society cares growth of the biomass feedstock. Because CO2 about. I argue that the absence of broad, from the combustion of fossil fuels, such as oil, meaningful metrics for climate-change, water-use, is one of the largest sources of anthropogenic and land-use impacts makes overall evaluations climate-active “greenhouse gases” (GHGs), it difficult. -
Well Below 2 C: Mitigation Strategies for Avoiding Dangerous To
PERSPECTIVE Well below 2 °C: Mitigation strategies for avoiding dangerous to catastrophic climate changes PERSPECTIVE Yangyang Xua,1 and Veerabhadran Ramanathanb,1 Edited by Susan Solomon, Massachusetts Institute of Technology, Cambridge, MA, and approved August 11, 2017 (received for review November 9, 2016) The historic Paris Agreement calls for limiting global temperature rise to “well below 2 °C.” Because of uncertainties in emission scenarios, climate, and carbon cycle feedback, we interpret the Paris Agree- ment in terms of three climate risk categories and bring in considerations of low-probability (5%) high- impact (LPHI) warming in addition to the central (∼50% probability) value. The current risk category of dangerous warming is extended to more categories, which are defined by us here as follows: >1.5 °C as dangerous; >3 °C as catastrophic; and >5 °C as unknown, implying beyond catastrophic, including existential threats. With unchecked emissions, the central warming can reach the dangerous level within three decades, with the LPHI warming becoming catastrophic by 2050. We outline a three- lever strategy to limit the central warming below the dangerous level and the LPHI below the cata- strophic level, both in the near term (<2050) and in the long term (2100): the carbon neutral (CN) lever to achieve zero net emissions of CO2, the super pollutant (SP) lever to mitigate short-lived climate pollutants, and the carbon extraction and sequestration (CES) lever to thin the atmospheric CO2 blan- ket. Pulling on both CN and SP levers and bending the emissions curve by 2020 can keep the central warming below dangerous levels. To limit the LPHI warming below dangerous levels, the CES lever must be pulled as well to extract as much as 1 trillion tons of CO2 before 2100 to both limit the preindustrial to 2100 cumulative net CO2 emissions to 2.2 trillion tons and bend the warming curve to a cooling trend. -
A Prediction Market for Climate Outcomes
Florida State University College of Law Scholarship Repository Scholarly Publications 2011 A Prediction Market for Climate Outcomes Shi-Ling Hsu Florida State University College of Law Follow this and additional works at: https://ir.law.fsu.edu/articles Part of the Environmental Law Commons, Law and Politics Commons, Natural Resources Law Commons, and the Oil, Gas, and Mineral Law Commons Recommended Citation Shi-Ling Hsu, A Prediction Market for Climate Outcomes, 83 U. COLO. L. REV. 179 (2011), Available at: https://ir.law.fsu.edu/articles/497 This Article is brought to you for free and open access by Scholarship Repository. It has been accepted for inclusion in Scholarly Publications by an authorized administrator of Scholarship Repository. For more information, please contact [email protected]. A PREDICTION MARKET FOR CLIMATE OUTCOMES * SHI-LING HSU This Article proposes a way of introducing some organization and tractability in climate science, generating more widely credible evaluations of climate science, and imposing some discipline on the processing and interpretation of climate information. I propose a two-part policy instrument consisting of (1) a carbon tax that is indexed to a “basket” of climate outcomes, and (2) a cap-and- trade system of emissions permits that can be redeemed in the future in lieu of paying the carbon tax. The amount of the carbon tax in this proposal (per ton of CO2) would be set each year on the basis of some objective, non-manipulable climate indices, such as temperature and mean sea level, and also on the number of certain climate events, such as flood events or droughts, that occurred in the previous year (or some moving average of previous years). -
A Cultural Analysis of a Physicist ''Trio'' Supporting the Backlash Against
ARTICLE IN PRESS Global Environmental Change 18 (2008) 204–219 www.elsevier.com/locate/gloenvcha Experiences of modernity in the greenhouse: A cultural analysis of a physicist ‘‘trio’’ supporting the backlash against global warming Myanna Lahsenà Center for Science and Technology Policy Research, University of Colorado and Instituto Nacional de Pesquisas Epaciais (INPE), Av. dos Astronautas, 1758, Sa˜o Jose´ dos Campos, SP 12227-010 Brazil Received 18 March 2007; received in revised form 5 October 2007; accepted 29 October 2007 Abstract This paper identifies cultural and historical dimensions that structure US climate science politics. It explores why a key subset of scientists—the physicist founders and leaders of the influential George C. Marshall Institute—chose to lend their scientific authority to this movement which continues to powerfully shape US climate policy. The paper suggests that these physicists joined the environmental backlash to stem changing tides in science and society, and to defend their preferred understandings of science, modernity, and of themselves as a physicist elite—understandings challenged by on-going transformations encapsulated by the widespread concern about human-induced climate change. r 2007 Elsevier Ltd. All rights reserved. Keywords: Anti-environmental movement; Human dimensions research; Climate change; Controversy; United States; George C. Marshall Institute 1. Introduction change itself, what he termed a ‘‘strong theory of culture.’’ Arguing that the essential role of science in our present age Human Dimensions Research in the area of global only can be fully understood through examination of environmental change tends to integrate a limited con- individuals’ relationships with each other and with ‘‘mean- ceptualization of culture. -
2012 Redacted Response
From: Gillis, Justin To: Andrew Dessler Subject: RE: thoughts on Heartland Leak w.r.t. cloud feedback Date: Thursday, March 08, 2012 11:23:54 AM Yes, he was making that complaint. "My papers get special treatment from the cabal," etc. etc. I have to say I read the reviews of the '11 paper, at your suggestion, and they looked completely professional and on-point to my unpracticed eye. -----Original Message----- From: On Behalf Of Andrew Dessler Sent: Thursday, March 08, 2012 12:07 PM To: Gillis, Justin Subject: Re: thoughts on Heartland Leak w.r.t. cloud feedback He's been trying to publish this, but it's been rejected at least twice and a third rejection is on the way (I think). Dick doesn't understand R^2 or, more likely, the argument is just a squirt of squids' ink designed to confuse. On Thu, Mar 8, 2012 at 10:20 AM, Gillis, Justin wrote: > He had choice words to say about your paper, by the way. "R-squared of .02! Can you believe that!" I take it that means he didn't like the width of your error bars, or some such... > > > > -----Original Message----- > From: On > Behalf Of Andrew Dessler > Sent: Thursday, March 08, 2012 11:18 AM > To: Gillis, Justin > Subject: Re: thoughts on Heartland Leak w.r.t. cloud feedback > >> I trust you're treating these e-mails in strictest confidence, as I will. > > yes, do not worry. > >> >> >> >> -----Original Message----- >> From: On >> Behalf Of Andrew Dessler >> Sent: Thursday, March 08, 2012 10:59 AM >> To: Gillis, Justin >> Subject: Re: thoughts on Heartland Leak w.r.t.