Global Climate Control: Is There a Better Strategy Than Reducing Greenhouse Gas Emissions?
Total Page:16
File Type:pdf, Size:1020Kb

Load more
Recommended publications
-
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). -
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). -
Fundamentals of Global Warming Science (PCC 587): Midterm Review
Fundamentals of Global Warming Science (PCC 587): Midterm Review DARGAN M. W. FRIERSON UNIVERSITY OF WASHINGTON, DEPARTMENT OF ATMOSPHERIC SCIENCES DAY 13: 11/6/12 The Instrumental Temperature Record Global temperature since 1880 Stevenson screens to measure temps on land, ocean temps from buckets or intake. Groups attempt to remove inhomogeneity in the datasets Other signs of (global) warming - melting mountain glaciers - decrease in winter snow cover - increasing atmospheric water vapor - warming of global oceans - warming of upper atmosphere - rising sea level (due to warming and ice-melt) - timing of seasonal events e.g. earlier thaws, later frosts - thinning and disappearing Arctic sea ice Every one of these data sets can be questioned to some extent. " Taken together, the totality of evidence of global warming is quite convincing." Solar vs Terrestrial Radiation Solar (blue) vs terrestrial (red) radiation: Very little overlap: solar (“shortwave”) and Earth (“longwave”) Solar Radiation and Earth When the Sun’s radiation reaches the Earth’s atmosphere, several things can happen: ¡ Scattering/reflection of solar radiation ¡ Absorption ¡ Transmission Most solar radiation makes it straight to the surface ¡ 50% of top-of-atmosphere (TOA) radiation is absorbed at the surface ¡ 20% is absorbed in atmosphere (17% in troposphere, 3% in stratosphere) ¡ 30% is reflected back to space (25% by atmosphere, 5% by surface) What does the reflection? Clouds reflect the most solar radiation by far ¡ 2/3 reflection by clouds ¡ 1/6 reflection by -
Mackenzie Climate Change Testimony
WRITTEN TESTIMONY OF FRED T. MACKENZIE, PH.D. DEPARTMENT OF OCEANOGRAPHY SCHOOL OF OCEAN AND EARTH SCIENCE AND TECHNOLOGY UNIVERSITY OF HAWAI‘I HEARING ON CLIMATE CHANGE IMPACTS AND RESPONSES IN ISLAND COMMUNITIES BEFORE THE SENATE COMMITTEE ON COMMERCE, SCIENCE, AND TRANSPORTATION MARCH 19, 2008 Introduction Good morning Senator Inouye, members of the committee, ladies and gentlemen. Thank you for giving me the opportunity this morning to speak to you on global climate issues and how they might impact island communities. My name is Fred Mackenzie and I am an Emeritus Professor in the Department of Oceanography at the University of Hawai‘i. My research is quite broad in scope but focuses on the behavior of the Earth’s surface system of oceans, atmosphere, land, and sediments through geologic time and its future under the influence of humans, including the problems associated with greenhouse gas emissions to the atmosphere, global warming, and ocean acidification. I have been an academician for more than 45 years and published more than 250 scholarly publications, including six books and nine edited volumes in ocean, Earth and environmental science. Today you have asked me to comment on how climate change might affect island communities and on our recent work developing climate and sustainability case studies for Pacific island resources that can be used to educate and inform the community, including local decision makers. Many of my comments are derived from the report of the Pacific Islands Regional Assessment Group, for which I served as a member, entitled Preparing for a Changing Climate. The Potential Consequences of Climate Variability and Change (Shea et al., 2001), and the case study Climate Change, Water Resources, and Sustainability in the Pacific Basin: Emphasis on O‘ahu, Hawai‘i and Majuro Atoll, Republic of the Marshall Islands (Guidry and Mackenzie, 2006). -
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. -
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. -
Radiation Dimming and Decreasing Water Clarity Fuel Underwater
Science Bulletin 65 (2020) 1675–1684 Contents lists available at ScienceDirect Science Bulletin journal homepage: www.elsevier.com/locate/scib Article Radiation dimming and decreasing water clarity fuel underwater darkening in lakes ⇑ ⇑ Yunlin Zhang a,b, , Boqiang Qin a,b, , Kun Shi a,b, Yibo Zhang a,b, Jianming Deng a,b, Martin Wild c, Lin Li d, Yongqiang Zhou a,b, Xiaolong Yao a,b, Miao Liu a,b, Guangwei Zhu a,b, Lu Zhang a,b, Binhe Gu e, Justin D. Brookes f a Taihu Laboratory for Lake Ecosystem Research, State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China b University of Chinese Academy of Sciences, Beijing 100049, China c Institute for Atmospheric and Climate Science, Zurich CH-8001, Switzerland d Department of Earth Sciences, Indiana University-Purdue University, Indianapolis IN 46202, USA e Soil and Water Science Department, University of Florida, Gainesville FL 32611, USA f Water Research Centre, Environment Institute, School of Biological Science, University of Adelaide, Adelaide 5005, Australia article info abstract Article history: Long-term decreases in the incident total radiation and water clarity might substantially affect the under- Received 30 January 2020 water light environment in aquatic ecosystems. However, the underlying mechanism and relative contri- Received in revised form 3 April 2020 butions of radiation dimming and decreasing water clarity to the underwater light environment on a Accepted 5 April 2020 national or global scale remains largely unknown. Here, we present a comprehensive dataset of unprece- Available online 16 June 2020 dented scale in China’s lakes to address the combined effects of radiation dimming and decreasing water clarity on underwater darkening. -
Ken Caldeira
Curriculum Vitae for Ken Caldeira PRESENT POSITION Senior Scientist Professor (by courtesy) Department of Global Ecology Department of Environmental Earth System Sciences Carnegie Institution Stanford University 260 Panama Street 450 Serra Mall Stanford, CA 94305 USA Stanford, California 94305 USA [email protected] [email protected] (650) 704-7212; fax: (650) 462-5968 EDUCATION Ph.D.,1991, New York University, Atmospheric Sciences, Department of Applied Science M.S.,1988, New York University, Atmospheric Sciences, Department of Applied Science B.A.,1978 Rutgers College, Philosophy PRIOR RESEARCH EXPERIENCE Physicist/Environmental Scientist (Lawrence Livermore National Laboratory, 1995 to 2005) Research ocean carbon cycle, atmospheric CO2, ocean/sea-ice physics, climate, and energy systems Post-Doctoral Researcher (Lawrence Livermore National Laboratory; 1993 to 1995) Research the ocean carbon cycle, atmospheric CO2 and climate NSF Earth Sciences Postdoctoral Fellow (Earth Systems Science Center & Dept. of Geosciences, The Pennsylvania State University; 1991 to 1993) Role of the carbonate-silicate cycle in long-term atmospheric CO2 content and climate GENERAL RESEARCH INTERESTS Ocean acidification; climate/carbon-cycle interactions; numerical simulation of climate and biogeochemistry; marine biogeochemical cycles; global carbon cycle; long-term evolution of climate and geochemical cycles; intentional intervention in the climate system; energy technology and policy ADVISORY PANELS / DISSERTATION COMMITTEES National Academy of Sciences, -
Global Dimming
Agricultural and Forest Meteorology 107 (2001) 255–278 Review Global dimming: a review of the evidence for a widespread and significant reduction in global radiation with discussion of its probable causes and possible agricultural consequences Gerald Stanhill∗, Shabtai Cohen Institute of Soil, Water and Environmental Sciences, ARO, Volcani Center, Bet Dagan 50250, Israel Received 8 August 2000; received in revised form 26 November 2000; accepted 1 December 2000 Abstract A number of studies show that significant reductions in solar radiation reaching the Earth’s surface have occurred during the past 50 years. This review analyzes the most accurate measurements, those made with thermopile pyranometers, and concludes that the reduction has globally averaged 0.51 0.05 W m−2 per year, equivalent to a reduction of 2.7% per decade, and now totals 20 W m−2, seven times the errors of measurement. Possible causes of the reductions are considered. Based on current knowledge, the most probable is that increases in man made aerosols and other air pollutants have changed the optical properties of the atmosphere, in particular those of clouds. The effects of the observed solar radiation reductions on plant processes and agricultural productivity are reviewed. While model studies indicate that reductions in productivity and transpiration will be proportional to those in radiation this conclusion is not supported by some of the experimental evidence. This suggests a lesser sensitivity, especially in high-radiation, arid climates, due to the shade tolerance of many crops and anticipated reductions in water stress. Finally the steps needed to strengthen the evidence for global dimming, elucidate its causes and determine its agricultural consequences are outlined. -
Fact Sheet on the Kyoto Protocol
The U.S. View FACT SHEET ON THE KYOTO PROTOCOL t a conference held December 1–11, 1997, in Kyoto, Japan, the Parties to A the UN Framework Convention on Climate Change agreed to an historic Protocol to reduce greenhouse gas emissions by harnessing the forces of the global marketplace to protect the environment. Key aspects of the Kyoto Protocol include weather, either of which could spike emissions targets, timetables for industrial- emissions in a particular year. ized nations, and market-based measures for meeting those targets. The Protocol • The first budget period will be makes a down payment on the meaning- 2008–2012. The parties rejected bud- ful participation of developing countries, get periods beginning as early as but more needs to be done in this area. 2003, as neither realistic nor achiev- Securing meaningful developing country able. Having a full decade before the participation remains a core U.S. goal. start of the binding period will allow more time for companies to make the transition to greater energy efficiency Emissions Targets and/or lower carbon technologies. A central feature of the Kyoto Protocol is a set of binding emissions targets for • The emissions targets include all six developed nations. The specific limits major greenhouse gases: carbon diox- vary from country to country, though ide, methane, nitrous oxide, and three those for the key industrial powers of the synthetic substitutes for ozone-deplet- European Union, Japan, and the United ing CFCs that are highly potent and States are similar—8 percent below 1990 long-lasting in the atmosphere. emissions levels for the European Union, 7 percent for the United States, and 6 • Activities that absorb carbon, such as percent for Japan. -
Emissions Gap Report 2018 © 2018 United Nations Environment Programme November 2018
Emissions Gap Report 2018 © 2018 United Nations Environment Programme November 2018 ISBN: 978-92-807-3726-4 Job number: DEW/2210/NA This publication may be reproduced in whole or in part and in any form for educational or non-profit services without special permission from the copyright holder, provided acknowledgement of the source is made. UN Environment would appreciate receiving a copy of any publication that uses this publication as a source. No use of this publication may be made for resale or any other commercial purpose whatsoever without prior permission in writing from UN Environment. Applications for such permission, with a statement of the purpose and extent of the reproduction, should be addressed to the Director, Communication Division, UN Environment, P. O. Box 30552, Nairobi 00100, Kenya. The designations employed and the presentation of the material in this publication do not imply the expression of any opinion whatsoever on the part of United Nations Environment Programme concerning the legal status of any country, territory or city or its authorities, or concerning the delimitation of its frontiers or boundaries. For general guidance on matters relating to the use of maps in publications please go to http://www.un.org/Depts/Cartographic/english/htmain.htm Disclaimers Mention of a commercial company or product in this document does not imply endorsement by UN Environment or the authors. The use of information from this document for publicity or advertising is not permitted. Trademark names and symbols are used in an editorial fashion with no intention on infringement of trademark or copyright laws. -
Ken Caldeira
Curriculum Vitae for Ken Caldeira PRESENT POSITION Senior Scientist Professor (by courtesy) Department of Global Ecology Department of Earth System Science Carnegie Institution Stanford University 260 Panama Street 450 Serra Mall Stanford, CA 94305 USA Stanford, California 94305 USA [email protected] [email protected] (650) 704-7212; fax: (650) 462-5968 EDUCATION Ph.D.,1991, New York University, Atmospheric Sciences, Department of Applied Science M.S.,1988, New York University, Atmospheric Sciences, Department of Applied Science B.A.,1978, Rutgers College, Philosophy PRIOR RESEARCH EXPERIENCE Physicist/Environmental Scientist (Lawrence Livermore National Laboratory, 1995 to 2005) Research ocean carbon cycle, atmospheric CO2, ocean/sea-ice physics, climate, and energy systems Post-Doctoral Researcher (Lawrence Livermore National Laboratory; 1993 to 1995) Research the ocean carbon cycle, atmospheric CO2 and climate NSF Earth Sciences Postdoctoral Fellow (Earth Systems Science Center & Dept. of Geosciences, The Pennsylvania State University; 1991 to 1993) Role of the carbonate-silicate cycle in long-term atmospheric CO2 content and climate GENERAL RESEARCH INTERESTS Ocean acidification; climate/carbon-cycle interactions; numerical simulation of climate and biogeochemistry; marine biogeochemical cycles; global carbon cycle; long-term evolution of climate and geochemical cycles; intentional intervention in the climate system; energy technology and policy ADVISORY PANELS / DISSERTATION COMMITTEES / ETC National Academy of Sciences, Geoengineering Climate Panel Member (2014) IPCC AR5 Report Climate Change 2013: The Physical Science Basis, Contributing Author (2013) Fellow of the American Geophysical Union (2010) National Academy of Sciences, America's Climate Choices Panel Member (2009) UK Royal Society Geoengineering Report Panel Member (2009) Global Carbon Project, Scientific Steering Committee Member (2009-2013) European Project on Ocean Acidification (EPOCA), Advisory Board Member (2008-2012) Intergovernmental Oceanographic Commission, Rep.