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TABLE OF CONTENTS
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April 2014 Volume 4, Issue 4 |
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| Editorial Correspondence Commentaries Feature Market Watch Research Highlights News and Views Perspectives Letters Article | |
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Editorial | Top |
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Carbon bubble toil and trouble p229 doi:10.1038/nclimate2193 Even if some sceptics consider climate science akin to witchcraft and politicians pursue ineffective policies, private enterprise is beginning to take climate change seriously. |
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Correspondence | Top |
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Upward adjustment needed for aerosol radiative forcing uncertainty pp230 - 232 Bjørn H. Samset, Gunnar Myhre and Michael Schulz doi:10.1038/nclimate2170 |
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Climate adaptation in India pp232 - 233 G. Dhanapal doi:10.1038/nclimate2114 |
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Temperature and drought effects on maize yield p233 Bruno Basso and Joe Ritchie doi:10.1038/nclimate2139 See also: Correspondence by David B. Lobell et al. |
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Reply to 'Temperature and drought effects on maize yield' p234 David B. Lobell, Graeme L. Hammer, Greg McLean, Carlos Messina, Michael J. Roberts and Wolfram Schlenker doi:10.1038/nclimate2140 See also: Correspondence by Bruno Basso et al. |
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Temperature and violence pp234 - 235 Mark A. Cane, Edward Miguel, Marshall Burke, Solomon M. Hsiang, David B. Lobell, Kyle C. Meng and Shanker Satyanath doi:10.1038/nclimate2171 |
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Commentaries | Top |
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Managing unnatural disaster risk from climate extremes pp235 - 237 Reinhard Mechler, Laurens M. Bouwer, Joanne Linnerooth-Bayer, Stefan Hochrainer-Stigler, Jeroen C. J. H. Aerts, Swenja Surminski and Keith Williges doi:10.1038/nclimate2137 Truly understanding climate-related disaster risk, and the management of that risk, can inform effective action on climate adaptation and the loss and damage mechanism, the main vehicle under the UN Climate Convention for dealing with climate-related effects, including residual impacts after adaptation. |
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Low-carbon investment risks and de-risking pp237 - 239 Tobias S. Schmidt doi:10.1038/nclimate2112 Effective mitigation of climate change requires investment flows to be redirected from high- to low-carbon technologies. However, especially in developing countries, low-carbon investments often suffer from high risks. More research is needed to address these risks and allow sound policy decisions to be made. |
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Feature | Top |
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Siphoning for safety p240 Bronwyn Wake doi:10.1038/nclimate2185 |
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Market Watch | Top |
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Investors take charge of climate policy pp241 - 242 Sonja van Renssen doi:10.1038/nclimate2175 When it comes to investments, the smart bet may be on clean energy and low-carbon infrastructure. Sonja van Renssen looks at the causes and implications of divestment from fossil fuels. |
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Research Highlights | Top |
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Scientific community: Reframing model priorities | Climate impacts: Cultural world heritage at risk | Ecological Impacts: Fly in the face of adversity | Climate modelling: Sensitivity to emissions | Psychology: Green choices motives |
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News and Views | Top |
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Perspectives | Top |
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A lower bound to the social cost of CO2 emissions pp253 - 258 J. C. J. M. van den Bergh and W. J. W. Botzen doi:10.1038/nclimate2135 Different estimates of the social cost of carbon make its translation to policy difficult. This Perspective evaluates past estimates of this cost and calculates a lower bound. Results show that dominant values for the social cost of carbon are gross underestimates and suggest that climate policy should be more stringent than previously proposed. |
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Social controversy belongs in the climate science classroom pp259 - 263 Elizabeth M. Walsh and Blakely K. Tsurusaki doi:10.1038/nclimate2143 Scientists, educators and stakeholders are grappling with how best to approach climate change education for diverse audiences, given the persistent social controversy associated with it. This Perspective examines how socio-cultural learning theories inform climate change education for learners with varied understanding of and attitudes towards climate change. |
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Letters | Top |
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Increasing stress on disaster-risk finance due to large floods pp264 - 268 Brenden Jongman, Stefan Hochrainer-Stigler, Luc Feyen, Jeroen C. J. H. Aerts, Reinhard Mechler, W. J. Wouter Botzen, Laurens M. Bouwer, Georg Pflug, Rodrigo Rojas and Philip J. Ward doi:10.1038/nclimate2124 An assessment of economic flood risk trends across Europe reveals high current and future stress on risk financing schemes. The magnitude and distribution of losses can be contained by investing in flood protection, increasing insurance coverage or by expanding public compensation funds. However, these climate change adaptation instruments have vastly different efficiency, equity and acceptability implications. Moreover, the spatial variation in disaster risk can necessitate cross-subsidies between individual countries in the European Union. |
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Vulnerability to the mortality effects of warm temperature in the districts of England and Wales pp269 - 273 James E. Bennett, Marta Blangiardo, Daniela Fecht, Paul Elliott and Majid Ezzati doi:10.1038/nclimate2123 Information about vulnerability to changes in temperature at the local level would improve the assessment of health risks created by climate change. Research now uses geo-coded data and spatial methods to quantify the effects of warm temperature on mortality for all districts in England and Wales. Mortality risk increases in southern districts by over 10% for a temperature increase of 1 °C, whereas northern districts are not significantly affected. |
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Inhomogeneous forcing and transient climate sensitivity pp274 - 277 Drew T. Shindell doi:10.1038/nclimate2136 Understanding how sensitive the climate is to different forcings is essential for projecting change. Analysis of results from climate model intercomparison projects shows that the climate has a greater sensitivity to aerosols and ozone compared with CO2. This result means that the low-range projections of climate response to CO2, <1.3 °C, are unlikely. See also: News and Views by David A. Stainforth |
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Cessation of deep convection in the open Southern Ocean under anthropogenic climate change pp278 - 282 Casimir de Lavergne, Jaime B. Palter, Eric D. Galbraith, Raffaele Bernardello and Irina Marinov doi:10.1038/nclimate2132 The Southern Ocean is a major site of open-ocean deep convection. Using observational data and model simulations, it is found that surface waters have freshened since the 1950s and deep convection has weakened, and could cease, as a result of the freshening. This has implications for bottom-water formation, ocean heat and carbon storage. See also: News and Views by Arnold L. Gordon |
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Fewer large waves projected for eastern Australia due to decreasing storminess pp283 - 286 Andrew J. Dowdy, Graham A. Mills, Bertrand Timbal and Yang Wang doi:10.1038/nclimate2142 Large ocean waves are predominantly caused by winds associated with extratropical cyclones. However, these winds are poorly represented in current global climate models, making wave projection difficult. A statistical study of large wave occurence in eastern Australia is applied to different climate models, allowing conclusions to be drawn about anthropogenic influence and improving wave projections. |
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A meta-analysis of crop yield under climate change and adaptation pp287 - 291 A. J. Challinor, J. Watson, D. B. Lobell, S. M. Howden, D. R. Smith and N. Chhetri doi:10.1038/nclimate2153 A comprehensive summary of studies that simulate climate change impacts on agriculture are now reported in a meta-analysis. Findings suggest that, without measures to adapt to changing conditions, aggregate yield losses should be expected for wheat, rice and maize in temperate and tropical growing regions even under relatively moderate levels of local warming. See also: News and Views by Reimund P. Rötter |
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Article | Top |
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Sustained mass loss of the northeast Greenland ice sheet triggered by regional warming pp292 - 299 Shfaqat A. Khan, Kurt H. Kjær, Michael Bevis, Jonathan L. Bamber, John Wahr, Kristian K. Kjeldsen, Anders A. Bjørk, Niels J. Korsgaard, Leigh A. Stearns, Michiel R. van den Broeke, Lin Liu, Nicolaj K. Larsen and Ioana S. Muresan doi:10.1038/nclimate2161 The Greenland ice sheet is a large contributor to sea-level rise primarily because of the increased speed of its glaciers in the southeast and northwest. This study looks at a previously stable ice stream in northeast Greenland, and finds that it is thinning due to regional warming. This region drains 16% of the ice sheet but has not figured in model projections of sea-level rise, indicating an under-estimation of Greenland contributions. |
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