The Rise and Fall of the Hockey Stick
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Andrew Montford's the Hockey Stick Illusion Is One of the Best Science
Andrew Montford‘s The Hockey Stick Illusion is one of the best science books in years. It exposes in delicious detail, datum by datum, how a great scientific mistake of immense political weight was perpetrated, defended and camouflaged by a scientific establishment that should now be red with shame. It is a book about principal components, data mining and confidence intervals—subjects that have never before been made thrilling. It is the biography of a graph. I can remember when I first paid attention to the ―hockey stick‖ graph at a conference in Cambridge. The temperature line trundled along with little change for centuries, then shot through the roof in the 20th century, like the blade of an ice-hockey stick. I had become somewhat of a sceptic about the science of climate change, but here was emphatic proof that the world was much warmer today; and warming much faster than at any time in a thousand years. I resolved to shed my doubts. I assumed that since it had been published in Nature—the Canterbury Cathedral of scientific literature—it was true. I was not the only one who was impressed. The graph appeared six times in the Intergovernmental Panel on Climate Change (IPCC)‘s third report in 2001. It was on display as a backdrop at the press conference to launch that report. James Lovelock pinned it to his wall. Al Gore used it in his film (though describing it as something else and with the Y axis upside down). Its author shot to scientific stardom. ―It is hard to overestimate how influential this study has been,‖ said the BBC. -
Supreme Court of the United States
No. 18-1451 ================================================================ In The Supreme Court of the United States --------------------------------- --------------------------------- NATIONAL REVIEW, INC., Petitioner, v. MICHAEL E. MANN, Respondent. --------------------------------- --------------------------------- On Petition For A Writ Of Certiorari To The District Of Columbia Court Of Appeals --------------------------------- --------------------------------- MOTION FOR LEAVE TO FILE BRIEF OF AMICUS CURIAE AND BRIEF OF AMICUS CURIAE SOUTHEASTERN LEGAL FOUNDATION IN SUPPORT OF PETITIONER --------------------------------- --------------------------------- KIMBERLY S. HERMANN HARRY W. MACDOUGALD SOUTHEASTERN LEGAL Counsel of Record FOUNDATION CALDWELL, PROPST & 560 W. Crossville Rd., Ste. 104 DELOACH, LLP Roswell, GA 30075 Two Ravinia Dr., Ste. 1600 Atlanta, GA 30346 (404) 843-1956 hmacdougald@ cpdlawyers.com Counsel for Amicus Curiae June 2019 ================================================================ COCKLE LEGAL BRIEFS (800) 225-6964 WWW.COCKLELEGALBRIEFS.COM 1 MOTION FOR LEAVE TO FILE BRIEF OF AMICUS CURIAE Pursuant to Supreme Court Rule 37.2, Southeast- ern Legal Foundation (SLF) respectfully moves for leave to file the accompanying amicus curiae brief in support of the Petition. Petitioner has consented to the filing of this amicus curiae brief. Respondent Michael Mann has withheld consent to the filing of this amicus curiae brief. Accordingly, this motion for leave to file is necessary. SLF is a nonprofit, public interest law firm and policy center founded in 1976 and organized under the laws of the State of Georgia. SLF is dedicated to bring- ing before the courts issues vital to the preservation of private property rights, individual liberties, limited government, and the free enterprise system. SLF regularly appears as amicus curiae before this and other federal courts to defend the U.S. Consti- tution and the individual right to the freedom of speech on political and public interest issues. -
Climate Change: Examining the Processes Used to Create Science and Policy, Hearing
CLIMATE CHANGE: EXAMINING THE PROCESSES USED TO CREATE SCIENCE AND POLICY HEARING BEFORE THE COMMITTEE ON SCIENCE, SPACE, AND TECHNOLOGY HOUSE OF REPRESENTATIVES ONE HUNDRED TWELFTH CONGRESS FIRST SESSION THURSDAY, MARCH 31, 2011 Serial No. 112–09 Printed for the use of the Committee on Science, Space, and Technology ( Available via the World Wide Web: http://science.house.gov U.S. GOVERNMENT PRINTING OFFICE 65–306PDF WASHINGTON : 2011 For sale by the Superintendent of Documents, U.S. Government Printing Office Internet: bookstore.gpo.gov Phone: toll free (866) 512–1800; DC area (202) 512–1800 Fax: (202) 512–2104 Mail: Stop IDCC, Washington, DC 20402–0001 COMMITTEE ON SCIENCE, SPACE, AND TECHNOLOGY HON. RALPH M. HALL, Texas, Chair F. JAMES SENSENBRENNER, JR., EDDIE BERNICE JOHNSON, Texas Wisconsin JERRY F. COSTELLO, Illinois LAMAR S. SMITH, Texas LYNN C. WOOLSEY, California DANA ROHRABACHER, California ZOE LOFGREN, California ROSCOE G. BARTLETT, Maryland DAVID WU, Oregon FRANK D. LUCAS, Oklahoma BRAD MILLER, North Carolina JUDY BIGGERT, Illinois DANIEL LIPINSKI, Illinois W. TODD AKIN, Missouri GABRIELLE GIFFORDS, Arizona RANDY NEUGEBAUER, Texas DONNA F. EDWARDS, Maryland MICHAEL T. MCCAUL, Texas MARCIA L. FUDGE, Ohio PAUL C. BROUN, Georgia BEN R. LUJA´ N, New Mexico SANDY ADAMS, Florida PAUL D. TONKO, New York BENJAMIN QUAYLE, Arizona JERRY MCNERNEY, California CHARLES J. ‘‘CHUCK’’ FLEISCHMANN, JOHN P. SARBANES, Maryland Tennessee TERRI A. SEWELL, Alabama E. SCOTT RIGELL, Virginia FREDERICA S. WILSON, Florida STEVEN M. PALAZZO, Mississippi HANSEN CLARKE, Michigan MO BROOKS, Alabama ANDY HARRIS, Maryland RANDY HULTGREN, Illinois CHIP CRAVAACK, Minnesota LARRY BUCSHON, Indiana DAN BENISHEK, Michigan VACANCY (II) C O N T E N T S Thursday, March 31, 2011 Page Witness List ............................................................................................................ -
Volume 2: Issues Raised by Petitioners on EPA's Use of IPCC
EPA’s Response to the Petitions to Reconsider the Endangerment and Cause or Contribute Findings for Greenhouse Gases under Section 202(a) of the Clean Air Act Volume 2: Issues Raised by Petitioners on EPA’s Use of IPCC U.S. Environmental Protection Agency Office of Atmospheric Programs Climate Change Division Washington, D.C. 1 TABLE OF CONTENTS Page 2.0 Issues Raised by Petitioners on EPA’s Use of IPCC.................................................................6 2.1 Claims That IPCC Errors Undermine IPCC Findings and Technical Support for Endangerment ........................................................................................................................6 2.1.1 Overview....................................................................................................................6 2.1.2 Accuracy of Statement on Percent of the Netherlands Below Sea Level..................8 2.1.3 Validity of Himalayan Glacier Projection .................................................................9 2.1.4 Characterization of Climate Change and Disaster Losses .......................................12 2.1.5 Validity of Alps, Andes, and African Mountain Snow Impacts..............................20 2.1.6 Validity of Amazon Rainforest Dieback Projection ................................................21 2.1.7 Validity of African Rain-Fed Agriculture Projection ..............................................23 2.1.8 Summary..................................................................................................................33 -
1 I Vestigati G Late Holoce E Orth Atla Tic Climate
S. Gaurin – dissertation prospectus UMass Geosciences IVESTIGATIG LATE HOLOCEE ORTH ATLATIC CLIMATE VARIABILITY THROUGH SPELEOTHEM PALEOPROXY AD HISTORICAL WEATHER DATA FROM BERMUDA INTRODUCTION Recent trends in hurricane frequency and intensity, a continually growing coastal population, and the presence of wide-reaching climatic patterns all underscore the importance of understanding changes in North Atlantic climate. Numerous paleoclimate studies have identified the North Atlantic as a region of importance in regulating global climate through meridional overturning circulation and other processes. The study proposed herein is focused on using stable isotope data from Bermuda speleothem calcium carbonate to help reconstruct dominant low-frequency modes of North Atlantic climate variability through the mid-Holocene (the last several thousand years). This period is replete with climate changes, from the warm hypsithermal peak of ~6000 years ago, followed by the slow overall cooling of the neoglacial, punctuated by rapid change “events” and century-scale periods like the Medieval Warm Period and Little Ice Age. Recent warming from the start of the 20 th century to the present has been attributed largely to the build-up of atmospheric greenhouse gases (Mann et al., 1998, 1999) and may herald the beginning of a possibly rapid transition to a new, warmer climate regime. The more we learn about the natural workings of the climate system on time scales of decades to centuries, which are of particular relevance as they are on the scale of a human lifetime, the better prepared we can be for warming-induced changes, some of which may already be afoot, such as the possibility that warmer ocean temperatures are increasing hurricane frequency (Goldenberg et al., 2001; Knight et al., 2006) or intensity (Knutson and Tuleya, 2004). -
Submission to the Garnaut Climate Change Review
2 January 2008 Submission from the Lavoisier Group to the Garnaut Climate Change Review Issues Paper 1 Climate Change: Land use – Agriculture and Forestry Abstract The economic history of Australia since 1788 has been characterised by some crucial turning points. John McArthur’s success in establishing the wool industry here in the early days of settlement was perhaps the most important. The discovery of gold in the 1850s was another. The establishment by Alfred Deakin, in the early years of federation, of a semi-closed economy was a tragic turning point. Contrariwise, the failure by Ben Chifley in 1946 to nationalise the banks was a very fortunate event, and the overturning by the Hawke Government of eighty years of protectionism has led to twenty years of continuing economic success. The threat of decarbonisation now hangs over Australia. If it is successfully imposed then the economic consequences will be similar to that which Chifley’s bank nationalisation ambitions would have had if they had been realised. In particular, if a cap and trade regime is imposed then, inexorably, governments will intrude more and more into economic decision making at the micro-level. The current trials of the German auto-manufacturers, as they battle the dictates of the bureaucrats in Brussels, provide a foretaste of the future under a cap-and-trade regime. There is no scientific consensus on the causal connection between anthropogenic carbon dioxide and global climate control. The weight of genuinely reputable scientific opinion is now firmly against any such connection. The best advice which the Garnaut Inquiry could offer the Rudd Government and the Australian people is that attributed to Bismarck - ‘Wait and See’. -
Red Lines & Hockey Sticks
Red Lines & Hockey Sticks A discourse analysis of the IPCC’s visual culture and climate science (mis)communication Thomas Henderson Dawson Department of ALM Theses within Digital Humanities Master’s thesis (two years), 30 credits, 2021, no. 5 Author Thomas Henderson Dawson Title Red Lines & Hockey Sticks: A discourse analysis of the IPCC’s visual culture and climate science (mis)communication. Supervisor Matts Lindström Abstract Within the climate science research community there exists an overwhelming consensus on the question of climate change. The scientific literature supports the broad conclusion that the Earth’s climate is changing, that this change is driven by human factors (anthropogenic), and that the environmental consequences could be severe. While a strong consensus exists in the climate science community, this is not reflected in the wider public or among poli- cymakers, where sceptical attitudes towards anthropogenic climate change is much more prevalent. This discrep- ancy in the perception of the urgency of the problem of climate change is an alarming trend and likely a result of a failure of science communication, which is the topic of this thesis. This paper analyses the visual culture of climate change, with specific focus on the data visualisations com- prised within the IPCC assessment reports. The visual aspects of the reports were chosen because of the prioriti- sation images often receive within scientific communication and for their quality as immutable mobiles that can transition between different media more easily than text. The IPCC is the central institutional authority in the climate science visual discourse, and its assessment reports, therefore, are the site of this discourse analysis. -
On the Climate History of Chaco Canyon
UC San Diego Scripps Institution of Oceanography Technical Report Title On the Climate History of Chaco Canyon Permalink https://escholarship.org/uc/item/1qv786mc Author Berger, Wolfgang H. Publication Date 2009-04-01 eScholarship.org Powered by the California Digital Library University of California ON THE CLIMATE HISTORY OF CHACO CANYON W.H. Berger, Ph.D. Scripps Institution of Oceanography University of California, San Diego Notes on Chaco Canyon history in connection with the presentation “Drought Cycles in Anasazi Land – Sun, Moon, and ocean oscillations,” at the PACLIM Conference in Asilomar, California, in April 2009. On the Involvement of the Sun in Chaco Canyon Climate History Tree-ring research since A.E. Douglass and E. Schulman has brought great benefits to the archaeology of the Southwest. It has become possible to reconstruct the climate narrative in some detail. The appropriate field of study is termed “dendroclimatology,” which is focused on the information contained in the growth of a given set of trees. The term harks back to the intent of the pioneer, the solar astronomer Douglass, who worked early in the 20th century. Since that time the study of tree rings has become a respected branch of Earth Sciences, with well-defined objects and methods (Hughes et al., 1982; Fritts, 1991). Douglass spent great efforts on documenting a role for the sun in climate change. Studies relating climate to solar variation have multiplied since. As yet, a focus on solar activity encounters much skepticism among climate scientists (see, e.g., Hoyt and Schatten, 1997). The expert’s skepticism has several causes. -
Medieval Warm Period’
WAS THERE A 'MEDIEVAL WARM PERIOD', AND IF SO, WHERE AND WHEN? MALCOLM K. HUGHES Laboratory of Tree Ring Research, University of Arizona, Tucson, AZ 85721 (addressfor correspondence), and Cooperative Institute for Research in Environmental Science, University of Colorado, Boulder, CO 80309, U.S.A. and HENRY F. DIAZ NOAA/ERL/CDC, 325 Broadway, Boulder, CO 80303, U.S.A. Abstract. It has frequently been suggested that the period encompassing the ninth to the fourteenth centuries A.D. experienced a climate warmer than that prevailing around the turn of the twentieth century. This epoch has become known as the Medieval Warm Period, since it coincides with the Middle Ages in Europe. In this review a number of lines of evidence are considered, (including climate- sensitive tree rings, documentary sources, and montane glaciers) in order to evaluate whether it is reasonable to conclude that climate in medieval times was, indeed, warmer than the climate of more recent times. Our review indicates that for some areas of the globe (for example, Scandinavia, China, the Sierra Nevada in California, the Canadian Rockies and Tasmania), temperatures, particularly in summer, appear to have been higher during some parts of this period than those that were to prevail until the most recent decades of the twentieth century. These warmer regional episodes were not strongly synchronous. Evidence from other regions (for example, the Southeast United States, southern Europe along the Mediterranean, and parts of South America) indicates that the climate during that time was little different to that of later times, or that warming, if it occurred, was recorded at a later time than has been assumed. -
Solar Cycles: Another Prediction
Solar Cycles another prediction by Miles Mathis March 6, 2020 On February 2, I posted charts of the upcoming Solar Cycles, including in-depth predictions for Cycle 25 and Cycle 26. I showed Cycle 26—which will peak in about 2037—would be similar in strength to Cycle 19, which peaked in 1957 and is the largest on record. That's the good news. The bad news is that the strength of the upcoming Cycles will tend to be fodder for the Global Warming frauds, and I predict they will use the trend to claim victory and continue the scare tactics, using them to sell various treasury dips and new taxes. Because what few have told you is that there is a correlation between global temperatures and longterm Solar Cycles. For instance, the Little Ice Age corresponds to the Maunder Minimum. Mid-20th century warming corresponds to strong Cycles in those decades, and cooling from the late 1950s to the 1990s also follows diminishing Solar Cycles. So a stronger Sun in the upcoming decades will likely lead to a real bump in global temperatures. Remember, the big scare in the 1970s was Global Cooling, when they were sucking from the treasury to respond to that conjob. When that failed to pan out and temperatures flattened, they decided to switch gears and sell the Global Warming scare instead. These people are salesmen and they always have to be selling something. This is not to say we don't have major environmental problems that require immediate action. We do. We have huge problems of pollution and environmental degradation caused by industry, military, government, corporate farming, and general modern lifestyles. -
Climate in Medieval Central Eurasia
Climate in Medieval Central Eurasia Thesis Presented in Partial Fulfillment of the Requirements for the Degree Master of Arts in the Graduate School of The Ohio State University By Henry Misa Graduate Program in History The Ohio State University 2020 Thesis Committee Scott C. Levi, Advisor John L. Brooke 1 Copyrighted by Henry Ray Misa 2020 2 Abstract This thesis argues that the methodology of environmental history, specifically climate history, can help reinterpret the economic and political history of Central Eurasia. The introduction reviews the scholarly fields of Central Eurasian history, Environmental history and, in brief, Central Eurasian Environmental history. Section one introduces the methods of climate history and discusses the broad outlines of Central Eurasian climate in the late Holocene. Section two analyzes the rise of the Khitan and Tangut dynasties in their climatic contexts, demonstrating how they impacted Central Eurasia during this period. Section three discusses the sedentary empires of the Samanid and Ghaznavid dynasties in the context of the Medieval Climate Anomaly. Section four discusses the rise of the first Islamic Turkic empires during the late 10th and 11th century. Section five discusses the Qarakhitai and the Jurchen in the 12th century in the context of the transitional climate regime between the Medieval Quiet Period and the early Little Ice Age. The conclusion summarizes the main findings and their implications for the study of Central Eurasian Climate History. This thesis discusses both long-term and short-term time scales; in many cases small-scale political changes and complexities impacted how the long-term patterns of climate change impacted regional economies. -
The Medieval Climate Anomaly in Antarctica
Palaeogeography, Palaeoclimatology, Palaeoecology 532 (2019) 109251 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Review article The Medieval Climate Anomaly in Antarctica T ⁎ Sebastian Lüninga, , Mariusz Gałkab, Fritz Vahrenholtc a Institute for Hydrography, Geoecology and Climate Sciences, Hauptstraße 47, 6315 Ägeri, Switzerland b Department of Geobotany and Plant Ecology, Faculty of Biology and Environmental Protection, University of Lodz, 12/16 Banacha Str., Lodz, Poland c Department of Chemistry, University of Hamburg, Martin-Luther-King-Platz 6, 20146 Hamburg, Germany ABSTRACT The Medieval Climate Anomaly (MCA) is a well-recognized climate perturbation in many parts of the world, with a core period of 1000–1200 CE. Here we are mapping the MCA across the Antarctic region based on the analysis of published palaeotemperature proxy data from 60 sites. In addition to the conventionally used ice core data, we are integrating temperature proxy records from marine and terrestrial sediment cores as well as radiocarbon ages of glacier moraines and elephant seal colonies. A generally warm MCA compared to the subsequent Little Ice Age (LIA) was found for the Subantarctic Islands south of the Antarctic Convergence, the Antarctic Peninsula, Victoria Land and central West Antarctica. A somewhat less clear MCA warm signal was detected for the majority of East Antarctica. MCA cooling occurred in the Ross Ice Shelf region, and probably in the Weddell Sea and on Filchner-Ronne Ice Shelf. Spatial distribution of MCA cooling and warming follows modern dipole patterns, as reflected by areas of opposing temperature trends. Main drivers of the multi-centennial scale climate variability appear to be the Southern Annular Mode (SAM) and El Niño-Southern Oscillation (ENSO) which are linked to solar activity changes by nonlinear dynamics.