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  • 1
    Publication Date: 2014-11-19
    Description: Anthropogenic global warming is driven by emissions of a wide variety of radiative forcers ranging from very short-lived climate forcers (SLCFs), like black carbon, to very long-lived, like CO2. These species are often released from common sources and are therefore intricately linked. However, for reasons of simplification, this CO2–SLCF linkage...
    Keywords: Sustainability Science
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 2
    Publication Date: 2011-02-16
    Description: Precipitation changes are a key driver of climate change impacts. On average, global precipitation is expected to increase with warming. However, model projections show that precipitation does not scale linearly with surface air temperature. Instead, global hydrological sensitivity, the relative change of global-mean precipitation per degree of global warming, seems to vary across different scenarios and even with time. Based on output from 20 coupled Atmosphere-Ocean-General-Circulation-Models for up to 7 different scenarios, we discuss to what extent these variations can be explained by changes in the tropospheric energy budget. Our analysis supports earlier findings that long- and shortwave absorbers initially decrease global-mean precipitation. Including these absorbers into a multivariate scaling approach allows to closely reproduce the simulated global-mean precipitation changes. We find a sensitivity of global-mean precipitation to tropospheric greenhouse gas forcing of −0.42 ± 0.23%/(W/m2) (uncertainty given as one std of inter-model variability) and to black carbon emissions of −0.07 ± 0.02%/(Mt/yr). In combination with these two predictors the dominant longer-term effect of surface air temperatures on precipitation is estimated to be 2.2 ± 0.52%/K – much lower than the 6.5%/K that may be expected from the Clausius-Clapeyron relationship.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 3
    Publication Date: 2009-05-02
    Description: More than 100 countries have adopted a global warming limit of 2 degrees C or below (relative to pre-industrial levels) as a guiding principle for mitigation efforts to reduce climate change risks, impacts and damages. However, the greenhouse gas (GHG) emissions corresponding to a specified maximum warming are poorly known owing to uncertainties in the carbon cycle and the climate response. Here we provide a comprehensive probabilistic analysis aimed at quantifying GHG emission budgets for the 2000-50 period that would limit warming throughout the twenty-first century to below 2 degrees C, based on a combination of published distributions of climate system properties and observational constraints. We show that, for the chosen class of emission scenarios, both cumulative emissions up to 2050 and emission levels in 2050 are robust indicators of the probability that twenty-first century warming will not exceed 2 degrees C relative to pre-industrial temperatures. Limiting cumulative CO(2) emissions over 2000-50 to 1,000 Gt CO(2) yields a 25% probability of warming exceeding 2 degrees C-and a limit of 1,440 Gt CO(2) yields a 50% probability-given a representative estimate of the distribution of climate system properties. As known 2000-06 CO(2) emissions were approximately 234 Gt CO(2), less than half the proven economically recoverable oil, gas and coal reserves can still be emitted up to 2050 to achieve such a goal. Recent G8 Communiques envisage halved global GHG emissions by 2050, for which we estimate a 12-45% probability of exceeding 2 degrees C-assuming 1990 as emission base year and a range of published climate sensitivity distributions. Emissions levels in 2020 are a less robust indicator, but for the scenarios considered, the probability of exceeding 2 degrees C rises to 53-87% if global GHG emissions are still more than 25% above 2000 levels in 2020.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Meinshausen, Malte -- Meinshausen, Nicolai -- Hare, William -- Raper, Sarah C B -- Frieler, Katja -- Knutti, Reto -- Frame, David J -- Allen, Myles R -- England -- Nature. 2009 Apr 30;458(7242):1158-62. doi: 10.1038/nature08017.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Potsdam Institute for Climate Impact Research, Telegraphenberg, 14412 Potsdam, Germany. malte.meinshausen@pik-potsdam.de〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19407799" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/chemistry ; Carbon Dioxide/analysis ; Ecology/*methods ; Forecasting ; Fossil Fuels/analysis ; *Greenhouse Effect ; *Models, Theoretical ; Probability ; *Temperature ; Uncertainty
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 4
    Publication Date: 2009-05-02
    Description: Global efforts to mitigate climate change are guided by projections of future temperatures. But the eventual equilibrium global mean temperature associated with a given stabilization level of atmospheric greenhouse gas concentrations remains uncertain, complicating the setting of stabilization targets to avoid potentially dangerous levels of global warming. Similar problems apply to the carbon cycle: observations currently provide only a weak constraint on the response to future emissions. Here we use ensemble simulations of simple climate-carbon-cycle models constrained by observations and projections from more comprehensive models to simulate the temperature response to a broad range of carbon dioxide emission pathways. We find that the peak warming caused by a given cumulative carbon dioxide emission is better constrained than the warming response to a stabilization scenario. Furthermore, the relationship between cumulative emissions and peak warming is remarkably insensitive to the emission pathway (timing of emissions or peak emission rate). Hence policy targets based on limiting cumulative emissions of carbon dioxide are likely to be more robust to scientific uncertainty than emission-rate or concentration targets. Total anthropogenic emissions of one trillion tonnes of carbon (3.67 trillion tonnes of CO(2)), about half of which has already been emitted since industrialization began, results in a most likely peak carbon-dioxide-induced warming of 2 degrees C above pre-industrial temperatures, with a 5-95% confidence interval of 1.3-3.9 degrees C.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Allen, Myles R -- Frame, David J -- Huntingford, Chris -- Jones, Chris D -- Lowe, Jason A -- Meinshausen, Malte -- Meinshausen, Nicolai -- England -- Nature. 2009 Apr 30;458(7242):1163-6. doi: 10.1038/nature08019.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Department of Physics, University of Oxford, OX1 3PU, UK. myles.allen@physics.ox.ac.uk〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/19407800" target="_blank"〉PubMed〈/a〉
    Keywords: Atmosphere/*chemistry ; Benchmarking ; Carbon/*analysis ; Carbon Dioxide/*analysis ; Computer Simulation ; *Greenhouse Effect ; History, 18th Century ; History, 19th Century ; History, 20th Century ; History, 21st Century ; Human Activities/history ; Industry/history ; *Models, Theoretical ; *Temperature ; Time Factors ; Uncertainty
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 5
    Publication Date: 2010-04-24
    Description: 〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Rogelj, Joeri -- Nabel, Julia -- Chen, Claudine -- Hare, William -- Markmann, Kathleen -- Meinshausen, Malte -- Schaeffer, Michiel -- Macey, Kirsten -- Hohne, Niklas -- England -- Nature. 2010 Apr 22;464(7292):1126-8. doi: 10.1038/4641126a.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Potsdam Institute for Climate Impact Research, 14473 Potsdam, Germany.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/20414291" target="_blank"〉PubMed〈/a〉
    Keywords: Carbon Dioxide/isolation & purification ; Forestry/trends ; Global Warming/*prevention & control/*statistics & numerical data ; *Goals ; *International Cooperation
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 6
    Publication Date: 2013-01-04
    Description: For more than a decade, the target of keeping global warming below 2 degrees C has been a key focus of the international climate debate. In response, the scientific community has published a number of scenario studies that estimate the costs of achieving such a target. Producing these estimates remains a challenge, particularly because of relatively well known, but poorly quantified, uncertainties, and owing to limited integration of scientific knowledge across disciplines. The integrated assessment community, on the one hand, has extensively assessed the influence of technological and socio-economic uncertainties on low-carbon scenarios and associated costs. The climate modelling community, on the other hand, has spent years improving its understanding of the geophysical response of the Earth system to emissions of greenhouse gases. This geophysical response remains a key uncertainty in the cost of mitigation scenarios but has been integrated with assessments of other uncertainties in only a rudimentary manner, that is, for equilibrium conditions. Here we bridge this gap between the two research communities by generating distributions of the costs associated with limiting transient global temperature increase to below specific values, taking into account uncertainties in four factors: geophysical, technological, social and political. We find that political choices that delay mitigation have the largest effect on the cost-risk distribution, followed by geophysical uncertainties, social factors influencing future energy demand and, lastly, technological uncertainties surrounding the availability of greenhouse gas mitigation options. Our information on temperature risk and mitigation costs provides crucial information for policy-making, because it clarifies the relative importance of mitigation costs, energy demand and the timing of global action in reducing the risk of exceeding a global temperature increase of 2 degrees C, or other limits such as 3 degrees C or 1.5 degrees C, across a wide range of scenarios.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Rogelj, Joeri -- McCollum, David L -- Reisinger, Andy -- Meinshausen, Malte -- Riahi, Keywan -- England -- Nature. 2013 Jan 3;493(7430):79-83. doi: 10.1038/nature11787.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Institute for Atmospheric and Climate Science, ETH Zurich, Universitatstrasse 16, CH-8092 Zurich, Switzerland. joeri.rogelj@env.ethz.ch〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/23282364" target="_blank"〉PubMed〈/a〉
    Keywords: Conservation of Energy Resources/*methods/*trends ; Global Warming/economics/*prevention & control ; Models, Theoretical ; Politics ; *Probability ; *Temperature ; Uncertainty
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 7
    Publication Date: 2013-01-30
    Description: Comprehensive computer simulations show that coral reefs are likely to suffer extensive long-term degradation resulting from mass bleaching events even if the expected increase in global mean temperature can be kept well below 2 °C. Without major mitigation efforts to limit global warming significantly, the fate of coral reef ecosystems seems to be sealed. Nature Climate Change 3 165 doi: 10.1038/nclimate1674
    Print ISSN: 1758-678X
    Electronic ISSN: 1758-6798
    Topics: Geosciences
    Published by Springer Nature
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  • 8
    Publication Date: 2013-03-12
    Description: [1]  Episodic explosive volcanic eruptions are a natural part of the climate system, but are often omitted from AOGCM pre-industrial spin-up and control experiments. This omission imposes a negative bias on ocean heat uptake in simulations of the historical period. In models of a range of complexity, we find that global-mean sea-level rise due to thermal expansion during the last ~150 years is consequently underestimated by 5–30 mm, which is a substantial proportion of the model-mean of 50 mm in CMIP3 AOGCMs with anthropogenic forcing only, and is therefore important in accounting for 20th-century sea-level rise. We test and recommend a procedure for removing the bias.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 9
    Publication Date: 2016-12-13
    Description: Description unavailable
    Print ISSN: 1748-9318
    Electronic ISSN: 1748-9326
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering
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  • 10
    Publication Date: 2008-12-22
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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