Global Warming: Climate Orthodoxy Perpetuates a Hoax” Comes from an Oregonian Headline Writer
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2018 Energy & Environmental Newsletters
2018 Energy & Environmental Newsletters (1600± Studies, Reports & Articles on Energy, Environment, Education, etc.) The Alliance for Wise Energy Decisions (AWED) is an informal coalition of individuals and organizations interested in improving national, state, and local energy and environmental policies, world-wide. Our premise is that technical matters (like climate change, our energy options, etc.) should be addressed by using Real Science. (Please see WiseEnergy.org for more information). A key element of AWED’s efforts is public education. Towards that end, every 2-4 weeks we put together a Newsletter to try to balance what is found in the mainstream media about Energy and Environmental issues. (More recently we have also included articles about Science and Education.) We appreciate MasterResource for their assistance in publishing the Newsletters. Note 1: The Newsletters are intended to complement what’s on our website: WiseEnergy.org. Note 2: For links to other excellent sources of articles on Energy and Environmental matters please see the “Current News” page on our website. Note 3: The purpose of this extensive compilation is to make it easier to search for pertinent studies, reports and articles on a specific topic (e.g. wind energy interference with the military). It is advisable to try multiple search words — e.g. military, army, navy, etc. (Search terms are case insensitive over this HTML document.) Note 4: We originally verified that all the links below worked. — but over time these can change. If you find any errors, please email John Droz [aaprjohn at northnet dot org] and we will try to make corrections. -
Medieval Warm Period in South America
M EDIEVAL WARM PERIOD IN OUTH MERICA S A SPPI & CO2SCIENCE ORIGINAL PAPER ♦ September 4, 2013 MEDIEVAL WARM PERIOD IN SOUTH AMERICA Citation: Center for the Study of Carbon Dioxide and Global Change. "Medieval Warm Period in South America.” Last modified September 4, 2013. http://www.co2science.org/subject/m/summaries/mwpsoutham.php. Was there a Medieval Warm Period anywhere in addition to the area surrounding the North Atlantic Ocean, where its occurrence is uncontested? This question is of utmost importance to the ongoing global warming debate, since if there was, and if the locations where it occurred were as warm then as they are currently, there is no need to consider the temperature increase of the past century as anything other than the natural progression of the persistent millennial- scale oscillation of climate that regularly brings the earth several-hundred-year periods of modestly higher and lower temperatures that are totally independent of variations in atmospheric CO2 concentration. Hence, this question is here considered as it applies to South America, a region far removed from where the existence of the Medieval Warm Period was first recognized. Cioccale (1999) assembled what was known at the time about the climatic history of the central region of the country over the past 1400 years, highlighting a climatic "improvement" that began some 400 years before the start of the last millennium, which ultimately came to be characterized by "a marked increase of environmental suitability, under a relatively homogeneous climate." And as a result of this climatic amelioration that marked the transition of the region from the Dark Ages Cold Period to the Medieval Warm Period, Cioccale reported that "the population located in the lower valleys ascended to higher areas in the Andes," where they remained until around AD 1320, when the transition to the stressful and extreme climate of the Little Ice Age began. -
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). -
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 -
Using Patterns of Recurring Climate Cycles to Predict Future Climate Changes D.J
CHAPTER 21 Using Patterns of Recurring Climate Cycles to Predict Future Climate Changes D.J. Easterbrook Western Washington University, Bellingham, WA, United States OUTLINE 1. Introduction 395 4. Correlation of Temperature Cycles and the Pacific Decadal Oscillation 405 2. The Past is the Key to the Future: Lessons From Past Global Climate Changes 396 5. The Atlantic Multidecadal Oscillation 407 2.1 Past Climate Changes 396 6. Where Is Climate Headed During the Coming 2.2 Magnitude and Rate of Abrupt Climate Changes 396 Century? 407 2.3 Holocene Climate Changes (10,000 Years Ago 6.1 IPCC Predictions 407 to Present) 398 6.2 Predictions Based on Past Cyclic Climate 2.3.1 The Roman Warm Period 398 Patterns 407 2.3.2 Dark Ages Cool Period 398 2.3.3 Medieval Warm Period (900e1300 AD) 400 References 410 2.3.4 The Little Ice Age 401 2.3.5 Climate Changes During the Past Century 403 3. Significance of Past Global Climate Changes 404 1. INTRODUCTION Global warming that occurred from 1978 to about 1998 pushed climate change into the forefront of potential concern. Every day the news media is filled with dire predictions of impending disastersdcatastrophic melting of the Antarctic and Greenland ice sheets, drowning of major cities from sea level rise, drowning of major portions of countries, droughts, severe water shortages, no more snow, more extreme weather events (hurricanes, tor- nadoes), etc. With no unequivocal, cause-and-effect, tangible, physical evidence that increasing CO2 caused this most recent global warming, adherents of this ideology have had to rely on computer models that have proven to be unreliable. -
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 Science of Roman History Biology, Climate, and the Future of the Past
The Science of Roman History Biology, climaTe, and The fuTuRe of The PaST Edited by Walter Scheidel PRinceTon univeRSiTy PReSS PRinceTon & oxfoRd Copyright © 2018 by Princeton University Press Published by Princeton University Press, 41 William Street, Princeton, New Jersey 08540 In the United Kingdom: Princeton University Press, 6 Oxford Street, Woodstock, Oxfordshire OX20 1TR press.princeton.edu All Rights Reserved ISBN 978- 0- 691- 16256- 0 Library of Congress Control Number 2017963022 British Library Cataloging- in- Publication Data is available This book has been composed in Miller Printed on acid- free paper. ∞ Printed in the United States of America 10 9 8 7 6 5 4 3 2 1 conTenTS List of Illustrations and Tables · vii Notes on Contributors · ix Acknowledgments · xiii Maps · xiv Introduction 1 Walter Scheidel chaPTeR 1. Reconstructing the Roman Climate 11 Kyle Harper & Michael McCormick chaPTeR 2. Archaeobotany: The Archaeology of Human- Plant Interactions 53 Marijke van der Veen chaPTeR 3. Zooarchaeology: Reconstructing the Natural and Cultural Worlds from Archaeological Faunal Remains 95 Michael MacKinnon chaPTeR 4. Bones, Teeth, and History 123 Alessandra Sperduti, Luca Bondioli, Oliver E. Craig, Tracy Prowse, & Peter Garnsey chaPTeR 5. Human Growth and Stature 174 Rebecca Gowland & Lauren Walther chaPTeR 6. Ancient DNA 205 Noreen Tuross & Michael G. Campana chaPTeR 7. Modern DNA and the Ancient Mediterranean 224 Roy J. King & Peter A. Underhill Index · 249 [ v ] illuSTRaTionS and TaBleS Maps 1. Western Mediterranean. xiv 2. Eastern Mediterranean. xv 3. Northwestern Europe. xvi Figures 1.1. TSI (Total Solar Irradiance) from 14C. 19 1.2. TSI from 10Be. 19 1.3. -
1 U.S. National Aeronautics and Space Administration (NASA) Global Climate Change
1 U.S. National Aeronautics and Space Administration (NASA) Global Climate Change. https://climate.nasa.gov/vital-signs/arctic-sea-ice/ 2 Intergovernmental Panel for Climate Change (IPCC) First Assessment Report 1990, s 224. https://www.ipcc.ch/report/climate-change-the-ipcc-1990-and-1992-assessments/ 3 U.S. department of Energy, Projecting the Climatic Effects of Increasing Carbon Dioxide, December 1985, s 152. https://www.osti.gov/servlets/purl/5885458 4 Understanding Climate Change, A program for Action, National Academy of Sciences 1975, s. 148, https://ia801806.us.archive.org/7/items/understandingcli00unit/understandingcli00unit.pdf 5 Graf från Tony Heller, https://realclimatescience.com/2019/03/nasa-tampering-with-reykjavik-raw- temperature-data/. Aktuella temperaturdata för Reykjavik från NASA (justerade): https://data.giss.nasa.gov/cgi-bin/gistemp/stdata_show_v4.cgi?id=IC000004030&dt=1&ds=14 6 Ole Humlum, www.climate4you.com. Datakälla: HadCRUT4, Hadley Climate Research Unit, University of East Anglia. 7 Multisensor Analyzed Sea Ice Extent (MASIE) från National Ice Center (NIC) och Sea Ice Index (SII) från National Snow and Ice Data Center (NSIDC) tillhörande National Oceanic and Atmospheric Administration (NOAA). https://www.climatedepot.com/2019/10/02/2019-arctic-ice-demise-deferred- again/ 8 Pan-Arctic Ice Ocean Modeling and Assimilation System (PIOMAS) vid Polar Science Center. https://psc.apl.washington.edu/research/projects/arctic-sea-ice-volume-anomaly/ 9 United States Geological Survey. https://en.m.wikipedia.org/wiki/File:Glacierbaymap.gif 10 Jim Steele. https://www.youtube.com/watch?time_continue=270&v=UaZb0r4G_Gc 11 Jim Steele. https://www.youtube.com/watch?time_continue=270&v=UaZb0r4G_Gc 12 Polarportal. -
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 -
Oxygen Isotope Evidence for Paleoclimate Change During The
PALEOCLIMATE RECONSTRUCTION IN NORTHWEST SCOTLAND AND SOUTHWEST FLORIDA DURING THE LATE HOLOCENE Ting Wang A dissertation submitted to the faculty of the University of North Carolina at Chapel Hill in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Department of Geological Sciences. Chapel Hill 2011 Approved by: Dr. Donna M. Surge Dr. Joseph G. Carter Dr. Jose A. Rial Dr. Justin B. Ries Dr. Karen J. Walker © 2011 Ting Wang ALL RIGHTS RESERVED ii ABSTRACT TING WANG: Paleoclimate Reconstruction in Northwest Scotland and Southwest Florida during the Late Holocene (Under the direction of Dr. Donna M. Surge) The study reconstructed seasonal climate change in mid-latitude northwest Scotland during the climate episodes Neoglacial (~3300-2500 BP) and Roman Warm Period (RWP; ~2500-1600 BP) and in subtropical southwest Florida during the latter part of RWP (1-550 AD) based on archaeological shell accumulations in two study areas. In northwest Scotland, seasonal sea surface temperature (SST) during the Neoglacial and RWP was estimated from high-resolution oxygen isotope ratios (δ18O) of radiocarbon-dated limpet (Patella vulgata) shells accumulated in a cave dwelling on the Isle of Mull. The SST results revealed a cooling transition from the Neoglacial to RWP, which is supported by earlier studies of pine pollen in Scotland and European glacial events and also coincident with the abrupt climate deterioration at 2800-2700 BP. The cooling transition might have been driven by decreased solar radiation and weakened North Atlantic Oscillation (NAO) conditions. In southwest Florida, seasonal-scale climate conditions for the latter part of RWP were reconstructed by using high-resolution δ18O of archaeological shells (Mercenaria campechiensis) and otoliths (Ariopsis felis).