The Myth of the 1970S Global Cooling Scientific Consensus
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The Scientist, Spring 2008
San Jose State University SJSU ScholarWorks The Scientist (College of Science) College of Science Spring 1-1-2008 The Scientist, Spring 2008 San Jose State University, College of Science Follow this and additional works at: https://scholarworks.sjsu.edu/scientist Recommended Citation San Jose State University, College of Science, "The Scientist, Spring 2008" (2008). The Scientist (College of Science). 2. https://scholarworks.sjsu.edu/scientist/2 This Newsletter is brought to you for free and open access by the College of Science at SJSU ScholarWorks. It has been accepted for inclusion in The Scientist (College of Science) by an authorized administrator of SJSU ScholarWorks. For more information, please contact [email protected]. Volume 12, Number 1 Spring 2008 College of Science San José State University The Scientist Message from the Dean Inside this issue: It’s been a busy I am also very pleased to an- Message from the 1 year here at the College of nounce that Dr. Singmaster Dean Science. Building on the has been designated the Geology: 2 great work of a planning SJSU Professor of the Year, a The Millers We are very pleased team made up of faculty, well deserved honor recog- to welcome our new Develop- Michael Graham: staff, and students that met nizing her years of selfless ment officer, Carol Beattie, 2 Kelp Discovery at a retreat at Asilomar a dedication to our students, who joined the university ad- year ago, we have nearly as well as her remarkable vancement staff in January. Physics and finalized plans for a College- teaching abilities. Carol has extensive experi- Astronomy 3 wide advising center, which We are continuing to ence in industry, consulting 2007 Highlights we hope will turn into a one- develop Professional Science and working with non-profits stop-shop for students in all Master’s programs that are such as the Children’s Health Mathematics News 4 departments of the college. -
Sam White the Real Little Ice Age Between C.1300 and C.1850 A.D
Journal of Interdisciplinary History, xliv:3 (Winter, 2014), 327–352. THE REAL LITTLE ICE AGE Sam White The Real Little Ice Age Between c.1300 and c.1850 a.d. the world became, on average, slightly but signiªcantly colder. The change varied over time and space, and its causes remain un- certain. Nevertheless, this cooling constitutes a meaningful climate event, with signiªcant historical consequences. Both the cooling trend and its effects on humans appear to have been particularly Downloaded from http://direct.mit.edu/jinh/article-pdf/44/3/327/1706251/jinh_a_00574.pdf by guest on 28 September 2021 acute from the late sixteenth to the late seventeenth century in much of the Northern Hemisphere. This article explains why climatologists and historians are conªdent that these changes occurred. On close examination, the objections raised in this issue of the journal by Kelly and Ó Gráda turn out to be entirely unfounded. The proxy data for early mod- ern global cooling (such as tree rings and ice cores) are robust, and written weather descriptions and observations of physical phenom- ena (such as glacial movements and river freezings) by and large of- fer independent conªrmation. Kelly and Ó Gráda’s proposed alter- native measures of climate and climate change suffer from serious ºaws. As we review the evidence and refute their criticisms, it will become clear just how solid the case for the Little Ice Age (lia) has become. the case for the little ice age The evidence for early modern global cooling comes, ªrst and foremost, from extensive research into physical proxies, including ice cores, tree rings, corals, and speleothems (stalagmites and stalactites). -
Government: the View from Washington, DC
THIS IS THE TEXT OF AN ESSAY IN THE WEB SITE “THE DISCOVERY OF GLOBAL WARMING” BY SPENCER WEART, HTTP://WWW.AIP.ORG/HISTORY/CLIMATE. JULY 2007. HYPERLINKS WITHIN THAT SITE ARE NOT INCLUDED IN THIS FILE. FOR AN OVERVIEW SEE THE BOOK OF THE SAME TITLE (HARVARD UNIV. PRESS, 2003). COPYRIGHT © 2003-2007 SPENCER WEART & AMERICAN INSTITUTE OF PHYSICS. Government: The View from Washington, DC The money that paid for research on climate change came mostly from governments. Governments were also central to any practical actions that might address global warming. Following the Second World War, the United States Federal government funded many kinds of research, much of it connected to Cold War concerns, and some of this happened to relate to climate change. During the 1960s, the government created major agencies for space, atmospheric, and ocean science, and in the 1970s, as public concern for the environment mounted, the agencies increasingly supported research targeted directly at climate change. But climate scientists were too few and disorganized to push through a unified national research program. Their budgets, divided among different agencies, would rise for a few years and then stagnate. During the 1980s, the funding and the science itself came under attack. The technical question of whether climate change might be a threat got caught up in political battles between pro-regulation environmentalists and anti-government conservatives. Demands for policies to mitigate global warming found little support among American politicians, who thought the ideas were politically unfeasible if not downright pernicious. (This essay covers only the United States government—the most important by far, in terms of influence and domestic greenhouse gas production. -
Accommodating Climate Change Science: James Hansen and the Rhetorical/Political Emergence of Global Warming
Science in Context 26(1), 137–152 (2013). Copyright ©C Cambridge University Press doi:10.1017/S0269889712000312 Accommodating Climate Change Science: James Hansen and the Rhetorical/Political Emergence of Global War ming Richard D. Besel California Polytechnic State University E-mail: [email protected] Argument Dr. James Hansen’s 1988 testimony before the U.S. Senate was an important turning point in the history of global climate change. However, no studies have explained why Hansen’s scientific communication in this deliberative setting was more successful than his testimonies of 1986 and 1987. This article turns to Hansen as an important case study in the rhetoric of accommodated science, illustrating how Hansen successfully accommodated his rhetoric to his non-scientist audience given his historical conditions and rhetorical constraints. This article (1) provides a richer explanation for the rhetorical/political emergence of global warming as an important public policy issue in the United States during the late 1980s and (2) contributes to scholarly understanding of the rhetoric of accommodated science in deliberative settings, an often overlooked area of science communication research. Standing on the promontory of the rocky rims in Billings, Montana, there is usually a distinct horizontal line between the clear, blue sky and the white, snowcapped Beartooth Mountains. But the summer of 1988 was different. A fuzzy, reddish tint lingered across the once pristine skyline of “Big Sky Country.” The reason: More than one hundred miles to the south, Yellowstone National Park smoldered in one of the most devastating forest fires of the twentieth century (Anon. 1988, A18; Stevens 1999, 129–130). -
Reforestation in a High-CO2 World—Higher Mitigation Potential Than
Geophysical Research Letters RESEARCH LETTER Reforestation in a high-CO2 world—Higher mitigation 10.1002/2016GL068824 potential than expected, lower adaptation Key Points: potential than hoped for • We isolate effects of land use changes and fossil-fuel emissions in RCPs 1 1 1 1 •ClimateandCO2 feedbacks strongly Sebastian Sonntag , Julia Pongratz , Christian H. Reick , and Hauke Schmidt affect mitigation potential of reforestation 1Max Planck Institute for Meteorology, Hamburg, Germany • Adaptation to mean temperature changes is still needed, but extremes might be reduced Abstract We assess the potential and possible consequences for the global climate of a strong reforestation scenario for this century. We perform model experiments using the Max Planck Institute Supporting Information: Earth System Model (MPI-ESM), forced by fossil-fuel CO2 emissions according to the high-emission scenario • Supporting Information S1 Representative Concentration Pathway (RCP) 8.5, but using land use transitions according to RCP4.5, which assumes strong reforestation. Thereby, we isolate the land use change effects of the RCPs from those Correspondence to: of other anthropogenic forcings. We find that by 2100 atmospheric CO2 is reduced by 85 ppm in the S. Sonntag, reforestation model experiment compared to the reference RCP8.5 model experiment. This reduction is [email protected] higher than previous estimates and is due to increased forest cover in combination with climate and CO2 feedbacks. We find that reforestation leads to global annual mean temperatures being lower by 0.27 K in Citation: 2100. We find large annual mean warming reductions in sparsely populated areas, whereas reductions in Sonntag, S., J. -
The Dilemma of Reticence: Helmut Landsberg, Stephen Schneider, and Public Communication of Climate Risk, 1971-1976
History of Meteorology 6 (2014) 53 The Dilemma of Reticence: Helmut Landsberg, Stephen Schneider, and public communication of climate risk, 1971-1976 Gabriel Henderson Aarhus University Aarhus, Denmark “Most of the crucial issues of human survival that will confront humanity over the next few decades will call for ethical and political value judgments – decisions on how to act in the face of uncertainties. … Human value judgments are too important to be left exclusively to the experts.” – Stephen Schneider1 “Science is not as objective as some people think. Often human value judgments (or even prejudices) make things move as much as curiosity or the search for answers as to ‘why.’” – Helmut Landsberg2 During the tumultuous mid-1970s, when energy and food shortages, environmental pollution, and political instability induced suspicions that America was increasingly susceptible to increased climatic instability, American climatologists Helmut Landsberg and Stephen Schneider disagreed strongly on whether scientists should engage the public about the future risks and urgency of climate change. On the one hand, Schneider, a young climate modeler with the National Center for Atmospheric Research (NCAR), expressed explicitly an unwillingness to embrace reticence as an appropriate response to the risks of climate change. To illustrate the gravity of the situation, he frequently resorted to vivid and frightening metaphors to convince the public and policy makers that I want to express my gratitude to Ruth Morgan and the anonymous reviewer who contributed thoughtful suggestions to improve and refine the scope of this article. I would also like to thank my colleagues at the Center for Science Studies at Aarhus University for their suggestions to strengthen my narrative and flow of argument: Dania Achermann, Matthias Heymann, and Janet Martin-Nielsen. -
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 -
Global Climate Coalition Primer on Climate Change Science
~ ~ Chairman F.SOHWAB Poraohe TECH-96-29 1st Viae C".lrrn.n C. MAZZA 1/18/96 Hyundal 2nd Vic. Ohalrrnan C. SMITH Toyota P S_cret.ry C. HELFMAN TO: AIAM Technical Committee BMW Treasurer .,J.AMESTOY Mazda FROM: Gregory J. Dana Vice President and Technical Director BMW c ••woo Flat RE: GLOBAL CLIMATE COALITION-(GCC)· Primer on Honda Hyundal Climate Change Science· Final Draft lauzu Kia , Land Rover Enclosed is a primer on global climate change science developed by the Mazda Mlt8ublehl GCC. If any members have any comments on this or other GCC NIB.an documents that are mailed out, please provide me with your comments to Peugeot forward to the GCC. Poreche Renault RolI&-Aoyoe S ••b GJD:ljf ""al'"u .z.ukl Toyota VOlkswagen Volvo President P. HUTOHINSON ASSOCIATION OF INTERNATIONAL AUTOMOBILE MANUFACTURERS. INC. 1001 19TH ST. NORTH. SUITE 1200 • ARLINGTON, VA 22209. TELEPHONE 703.525.7788. FAX 703.525.8817 AIAM-050771 Mobil Oil Corporation ENVIRONMENTAL HEALTH AND SAFETY DEPARTh4ENT P.O. BOX1031 PRINCETON, NEW JERSEY 08543-1031 December 21, 1995 'To; Members ofGCC-STAC Attached is what I hope is the final draft ofthe primer onglobal climate change science we have been working on for the past few months. It has been revised to more directly address recent statements from IPCC Working Group I and to reflect comments from John Kinsman and Howard Feldman. We will be discussing this draft at the January 18th STAC meeting. Ifyou are coming to that meeting, please bring any additional comments on the draft with you. Ifyou have comments but are unable to attend the meeting, please fax them to Eric Holdsworth at the GeC office. -
News and Nntes
Bulletin American Meteorological Society pictures will be required to extract the wealth of data and tracked. The cloud systems comprising the Inter- on cloud developments, movements and dissipation. tropical Convergence Zone can be observed and studied. A preliminary analysis of the cloud observations from Tropical storms such as hurricanes and typhoons can ATS-I indicates that detailed viewing of short-lived be monitored continuously. The rapid changes associated weather systems and phenomena from synchronous alti- with storms and frontal systems can be readily observed tude is feasible. The observation of cloud systems over and assessed. The continuous monitoring of weather the tropical ocean will assist in the study of the heat systems from synchronous satellites will be an important budget of the atmosphere. Mesoscale phenomena such as adjunct to the ESS A and Nimbus satellites for observing thunderstorms, possibly even tornadoes, can be identified and studying the Earth's weather. news and nntes New institute director, University of Miami of Marine Science is planned with several joint appointments, common graduate courses in fluid dynamics, statistics, and Dr. Eric B. Kraus, formerly similar basic subjects, as well as access to research vessels and of Woods Hole Oceano- an instrumented field site for wave and air-sea interaction graphic Institution, has be- studies near Abaco Island in the Bahamas. come director of the Institute of Atmospheric Science, Uni- versity of Miami. He has also National Academy of Sciences building named been appointed professor of meteorology at the Univer- The new building being constructed for the National Acad- sity's Institute of Marine emy of Sciences on property of George Washington University Science. -
Beno Gutenberg
NATIONAL ACADEMY OF SCIENCES B E N O G U T E N B ER G 1889—1960 A Biographical Memoir by L E O N KNOP OFF Any opinions expressed in this memoir are those of the author(s) and do not necessarily reflect the views of the National Academy of Sciences. Biographical Memoir COPYRIGHT 1999 NATIONAL ACADEMIES PRESS WASHINGTON D.C. Courtesy of the California Institute of Technology Archives, Pasadena BENO GUTENBERG June 4, 1889–January 25, 1960 BY LEON KNOPOFF ENO GUTENBERG WAS THE foremost observational seismolo- Bgist of the twentieth century. He combined exquisite analysis of seismic records with powerful analytical, inter- pretive, and modeling skills to contribute many important discoveries of the structure of the solid Earth and its atmo- sphere. Perhaps his best known contribution was the pre- cise location of the core of the Earth and the identification of its elastic properties. Other major contributions include the travel-time curves; the discovery of very long-period seis- mic waves with large amplitudes that circle the Earth; the identification of differences in crustal structure between continents and oceans, including the discovery of a signifi- cantly thin crust in the Pacific; the discovery of a low-veloc- ity layer in the mantle (which he interpreted as the zone of decoupling of horizontal motions of the surficial parts from the deeper parts of the Earth); the creation of the magni- tude scale for earthquakes; the relation between magnitudes and energies for earthquakes; the famous universal magni- tude-frequency relation for earthquake distributions; the first density distribution for the mantle; the study of the tem- perature distribution in the Earth; the understanding of microseisms; and the structure of the atmosphere. -
Monsoon Intensification, Ocean Warming and Steric Sea Level Rise
Manuscript prepared for Earth Syst. Dynam. with version 3.2 of the LATEX class copernicus.cls. Date: 8 March 2011 Climate change under a scenario near 1.5◦C of global warming: Monsoon intensification, ocean warming and steric sea level rise Jacob Schewe1,2, Anders Levermann1,2, and Malte Meinshausen1 1Earth System Analysis, Potsdam Institute for Climate Impact Research, Potsdam, Germany 2Physics Institute, Potsdam University, Potsdam, Germany Abstract. We present climatic consequences of the Repre- 1 Introduction sentative Concentration Pathways (RCPs) using the coupled climate model CLIMBER-3α, which contains a statistical- In December 2010, the international community agreed, dynamical atmosphere and a three-dimensional ocean model. under the United Nations Framework Convention on Cli- We compare those with emulations of 19 state-of-the-art mate Change, to limit global warming to below 2◦C atmosphere-ocean general circulation models (AOGCM) us- (Cancun´ Agreements, see http://unfccc.int/files/meetings/ ing MAGICC6. The RCPs are designed as standard scenarios cop 16/application/pdf/cop16 lca.pdf). At the same time, it for the forthcoming IPCC Fifth Assessment Report to span was agreed that a review, to be concluded by 2015, should the full range of future greenhouse gas (GHG) concentra- look into a potential tightening of this target to 1.5◦C – in tions pathways currently discussed. The lowest of the RCP part because climate change impacts associated with 2◦C are scenarios, RCP3-PD, is projected in CLIMBER-3α to imply considered to exceed tolerable limits for some regions, e.g. a maximal warming by the middle of the 21st century slightly Small Island States. -
Global Cooling: the Little Ice Age the Concept of the Little Ice Age
GLOBAL WARMING: THE HOLOCENE -3- Helluland, today's Baffin Island, and sailed from there southwa d 0 a1;1o~her island that he called V~nland ('vineland'). About /o0~ V1km?s under Thorfinn Ka~lsefm even began to settle in North America. The sagas re~or? this, and we also have the evidence of the GLOBAL COOLING: THE LITTLE Anse au~ Meadows site m Newfoundland excavated in the 1960 ICE AGE From this settlement numbering more than one hundred inhabitant'' furth~r voyages w~r~ made to the south. But the hostility of th~ Skrrelmgs, as the V1kmgs called native Americans, led to the collapse of the first European colony in the Americas. The sea routes frorn Greenland, not to speak of Iceland or Norway were too distant t lend it support.162 ' o The Concept of the Little Ice Age The term 'Little Ice Age' was coined in the late 1930s by the US glaciologist Fram;ois Matthes (1875-1949). It first appeared in a report on recent glacier advances in North America, 1 then in the title of an essay on the geological interpretation of glacier moraines in the Yosemite valley. Matthes was interested in the coolings since the postglacial climatic optimum, that is, over the last three thousand years, and especially in that which followed the medieval warm period. In his view, most glaciers still existing in North America do not go back to the last great ice age but have arisen in this relatively short space of time. The period from the thirteenth to the nineteenth century, in which glaciers advanced in the Alps, Scandinavia and North America, he called 'the Little Ice Age' (to distinguish it from the great ice ages).