Science and the Precautionary Principle
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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). -
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. -
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. -
Increase in Domestic Electricity Consumption from Particulate Air Pollution
ARTICLES https://doi.org/10.1038/s41560-020-00699-0 Increase in domestic electricity consumption from particulate air pollution Pan He 1,2,6 ✉ , Jing Liang3,6, Yueming (Lucy) Qiu 3,6 ✉ , Qingran Li4 and Bo Xing5 Accurate assessment of environmental externalities of particulate air pollution is crucial to the design and evaluation of envi- ronmental policies. Current evaluations mainly focus on direct damages resulting from exposure, missing indirect co-damages that occur through interactions among the externalities, human behaviours and technologies. Our study provides an empirical assessment of such co-damages using customer-level daily and hourly electricity data of a large sample of residential and commercial consumers in Arizona, United States. We use an instrumental variable panel regression approach and find that par- ticulate matter air pollution increases electricity consumption in residential buildings as well as in retail and recreation service industries. Air pollution also reduces the actual electricity generated by distributed-solar panels. Lower-income and minority ethnic groups are disproportionally impacted by air pollution and pay higher electricity bills associated with pollution avoid- ance, stressing the importance of incorporating the consideration of environmental justice in energy policy-making. ir pollution has resulted in many types of negative externali- in commercial buildings for longer period of time. These two effects ties, a situation that calls for policy intervention to address can cancel out, and thus we hypothesize that air pollution does not Athe associated damages. Policymakers and research are have a statistically significant impact on commercial buildings as widely concerned with increases in mortality risk, which are direct a whole. -
Keeling Curve: Result, Interpretation & Global Monitoring
International Journal for Empirical Education and Research Keeling Curve: Result, Interpretation & Global Monitoring Augustyn Ostrowski Faculty of Geography & Geology Jagiellonian University Email: [email protected] (Author of Correspondence) Poland Abstract The Keeling Curve is a graph of the accumulation of carbon dioxide in the Earth's atmosphere based on continuous measurements taken at the Mauna Loa Observatory on the island of Hawaii from 1958 to the present day. The curve is named for the scientist Charles David Keeling, who started the monitoring program and supervised it until his death in 2005. Keywords: Mauna Loa Measurements; Results and Interpretation; Global Monitoring; Ralph Keeling. ISSN Online: 2616-4833 ISSN Print: 2616-4817 35 1. Introduction Keeling's measurements showed the first significant evidence of rapidly increasing carbon dioxide levels in the atmosphere. According to Dr Naomi Oreskes, Professor of History of Science at Harvard University, the Keeling curve is one of the most important scientific works of the 20th century. Many scientists credit the Keeling curve with first bringing the world's attention to the current increase of carbon dioxide in the atmosphere. Prior to the 1950s, measurements of atmospheric carbon dioxide concentrations had been taken on an ad hoc basis at a variety of locations. In 1938, engineer and amateur meteorologist Guy Stewart Callendar compared datasets of atmospheric carbon dioxide from Kew in 1898-1901, which averaged 274 parts per million by volume (ppm), and from the eastern United States in 1936-1938, which averaged 310 ppmv, and concluded that carbon dioxide concentrations were rising due to anthropogenic emissions. However, Callendar's findings were not widely accepted by the scientific community due to the patchy nature of the measurements. -
Global Climate Change Control: Is There a Better Strategy Than Reducing Greenhouse Gas Emissions?
GLOBAL CLIMATE CHANGE CONTROL: IS THERE A BETTER STRATEGY THAN REDUCING GREENHOUSE GAS EMISSIONS? † ALAN CARLIN This Article identifies four major global climate change problems, analyzes whether the most prominent of the greenhouse gas (GHG) control proposals is likely to be either effective or efficient in solving each of the problems, and then extensively analyzes both management and technological alternatives to the proposals. Efforts to reduce emissions of GHGs, such as carbon dioxide, in a decentralized way or even in a few countries (such as the United States or under the Kyoto Protocol) without equivalent actions by all the other countries of the world, particularly the most rapidly growing ones, cannot realistically achieve the temperature change limits most emission control advocates believe are neces- sary to avoid dangerous climatic changes, and would be unlikely to do so even with the cooperation of these other countries. This Article concludes that the most effective and efficient solution would be to use a concept long proven by nature to reduce the radiation reaching the earth by adding particles optimized for this purpose to the stratosphere to scatter a small portion of the incoming sunlight back into space, as well as to undertake a new effort to better under- stand and reduce ocean acidification. Current temperature change goals could be quickly achieved by stratospheric scattering at a very modest cost without the need for costly adaptation, human lifestyle changes, or the general public’s ac- tive cooperation, all required by rigorous emission controls. Although strato- spheric scattering would not reduce ocean acidification, for which several reme- dies are explored in this Article, it appears to be the most effective and efficient first step toward global climate change control. -
Environmental Effects of Ozone Depletion and Its Interactions with Climate Change: 2010 Assessment
University of Wollongong Research Online Faculty of Science - Papers (Archive) Faculty of Science, Medicine and Health 2010 Environmental Effects of Ozone Depletion and its Interactions with Climate Change: 2010 Assessment Sharon A. Robinson University of Wollongong, [email protected] Stephen R. Wilson University of Wollongong, [email protected] Follow this and additional works at: https://ro.uow.edu.au/scipapers Part of the Life Sciences Commons, Physical Sciences and Mathematics Commons, and the Social and Behavioral Sciences Commons Recommended Citation Robinson, Sharon A. and Wilson, Stephen R.: Environmental Effects of Ozone Depletion and its Interactions with Climate Change: 2010 Assessment 2010. https://ro.uow.edu.au/scipapers/456 Research Online is the open access institutional repository for the University of Wollongong. For further information contact the UOW Library: [email protected] Environmental Effects of Ozone Depletion and its Interactions with Climate Change: 2010 Assessment Abstract This quadrennial Assessment was prepared by the Environmental Effects Assessment Panel (EEAP) for the Parties to the Montreal Protocol. The Assessment reports on key findings on environment and health since the last full Assessment of 2006, paying attention to the interactions between ozone depletion and climate change. Simultaneous publication of the Assessment in the scientific literature aims to inform the scientific community how their data, modeling and interpretations are playing a role in information dissemination to the Parties -
Impact of Urbanization on Sunshine Duration from 1987 to 2016 in Hangzhou City, China
atmosphere Article Impact of Urbanization on Sunshine Duration from 1987 to 2016 in Hangzhou City, China Kai Jin 1,2,* , Peng Qin 1 , Chunxia Liu 1, Quanli Zong 1 and Shaoxia Wang 1,* 1 Qingdao Engineering Research Center for Rural Environment, College of Resources and Environment, Qingdao Agricultural University, Qingdao 266109, China; [email protected] (P.Q.); [email protected] (C.L.); [email protected] (Q.Z.) 2 State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Water and Soil Conservation, Northwest A&F University, Yangling 712100, China * Correspondence: [email protected] (K.J.); [email protected] (S.W.); Tel.: +86-150-6682-4968 (K.J.); +86-136-1642-9118 (S.W.) Abstract: Worldwide solar dimming from the 1960s to the 1980s has been widely recognized, but the occurrence of solar brightening since the late 1980s is still under debate—particularly in China. This study aims to properly examine the biases of urbanization in the observed sunshine duration series from 1987 to 2016 and explore the related driving factors based on five meteorological stations around Hangzhou City, China. The results inferred a weak and insignificant decreasing trend in annual mean sunshine duration (−0.09 h/d decade−1) from 1987 to 2016 in the Hangzhou region, indicating a solar dimming tendency. However, large differences in sunshine duration changes between rural, suburban, and urban stations were observed on the annual, seasonal, and monthly scales, which can be attributed to the varied urbanization effects. Using rural stations as a baseline, we found evident urbanization effects on the annual mean sunshine duration series at urban and suburban stations—particularly in the period of 2002–2016. -
Urbanization Effect on the Diurnal Temperature Range: Different Roles Under Solar Dimming and Brightening*
1022 JOURNAL OF CLIMATE VOLUME 25 Urbanization Effect on the Diurnal Temperature Range: Different Roles under Solar Dimming and Brightening* KAI WANG,HONG YE,FENG CHEN,YONGZHU XIONG, AND CUIPING WANG Key Laboratory of Urban Environment and Health, Institute of Urban Environment, Chinese Academy of Sciences, Xiamen, China (Manuscript received 28 December 2010, in final form 11 September 2011) ABSTRACT Based on the 1960–2009 meteorological data from 559 stations across China, the urbanization effect on the diurnal temperature range (DTR) was evaluated in this study. Different roles of urbanization were specially detected under solar dimming and solar brightening. During the solar dimming time, both urban and rural stations showed decreasing trends in maximum temperature (Tmax) because of decreased radiation, sug- gesting that the dimming effects are not only evident in urban areas but also in rural areas. However, mini- mum temperature (Tmin) increased more substantially in urban areas than in rural areas during the dimming period, resulting in a greater decrease in the DTR in the urban areas. When the radiation reversed from dimming to brightening, the change in the DTR became different. The Tmax increased faster in rural areas, suggesting that the brightening could be much stronger in rural areas than in urban areas. Similar trends of Tmin between urban and rural areas appeared during the brightening period. The urban DTR continued to show a decreasing trend because of the urbanization effect, while the rural DTR presented an increasing trend. The remarkable DTR difference in the urban and rural areas showed a significant urbanization effect in the solar brightening time. -
Fifty-Six Years of Surface Solar Radiation and Sunshine
1 Fifty-six years of Surface Solar Radiation and Sunshine 2 Duration at the Surface in over São Paulo, Brazil: 1961 3 - 2016 4 5 Marcia Akemi Yamasoe1, Nilton Manuel Évora do Rosário2, 6 Samantha Novaes Santos Martins Almeida 3, Martin Wild4 7 [1] Departamento de Ciências Atmosféricas, Instituto de Astronomia, Geofísica e 8 Ciências Atmosféricas, Universidade de São Paulo, São Paulo, Brazil 9 [2] Departamento de Ciências Ambientais, Universidade Federal de São Paulo, 10 Diadema, São Paulo, Brazil 11 [3] Seção de Serviços Meteorológicos do Instituto de Astronomia, Geofísica e Ciências 12 Atmosféricas, Universidade de São Paulo, São Paulo, Brazil 13 [4] Institute for Atmospheric and Climate Science, ETH Zurich, Switzerland 14 15 Correspondence to: M. A. Yamasoe ([email protected]) 16 1 17 18 Abstract 19 Fifty-six years (1961 – 2016) of daily surface downward solar irradiation, 20 sunshine duration, diurnal temperature range and the fraction of the sky covered by 21 clouds in the city of São Paulo, Brazil, were analyzed. The main purpose was to 22 contribute to the characterization and understanding of the dimming and brightening 23 effects on solar global radiation in this part of South America. As observed in most of 24 the previous studies worldwide, in this study, during the period between 1961 up to the -2 25 early 1980’s, more specifically up to 1983, a negative trend of about -0.40 kJm per Formatado: Não Realce 26 decade, with a significance level of p = 0.101 in surface solar irradiation was detected in 27 São Paulo, characterizing the occurrence of a dimming effect. -
Joshua P. Howe (Editor)
Isis Joshua P. Howe (Editor). Making Climate Change History. Documents from Global Warming's Past. --Manuscript Draft-- Manuscript Number: Full Title: Joshua P. Howe (Editor). Making Climate Change History. Documents from Global Warming's Past. Corresponding Author: Evan Hepler-Smith Duke University Durham, NC UNITED STATES Order of Authors Secondary Information: Powered by Editorial Manager® and ProduXion Manager® from Aries Systems Corporation Book Review Joshua P. Howe (Editor). Making Climate Change History. Documents from Global Warming's Past. Foreword by Paul S. Sutter. (Weyerhaeuser Environmental Classics.) xvi +340 pp., notes, index. Seattle: University of Washington Press, 2017. $24.00 (paper), ISBN 9780295741390. Making Climate Change History is a compilation of historical documents tracing the accumulation of scientific evidence regarding anthropogenic global warming and its consequences, as well as political controversy and (in)action based on the warnings of climate scientists. The bulk of the sources originate in American settings and perspectives. Ample historical scholarship tells this story; editor Joshua Howe mentions Spencer Weart’s The Discovery of Global Warming (Harvard, rev. ed. 2008), Naomi Oreskes and Eric Conway’s Merchants of Doubt (Bloomsbury, 2010), Jacob Hamblin’s Arming Mother Nature (Oxford, 2013), and Howe’s own Behind the Curve (University of Washington, 2014), among others. Howe presents the collection as the sources behind such stories and raw material for readers to fashion their own interpretive histories of climate change. The book is in six parts, each introduced by a short essay providing historical context and a series of questions to guide readers’ historical engagement with the sources. Part 1, “The Scientific ‘Prehistory’ of Global Warming,” runs from Joseph Fourier’s 1824 paper on the temperature of the earth through Guy Stewart Callendar’s 1938 article correlating the emission of carbon dioxide from fuel combustion with a long-term increase in atmospheric temperature.