Wednesday, March 26, 2014

Nature Climate Change Contents April 2014 Volume 4 Number 4 pp 229-299

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Nature Chemistry

TABLE OF CONTENTS

April 2014 Volume 4, Issue 4

Editorial
Correspondence
Commentaries
Feature
Market Watch
Research Highlights
News and Views
Perspectives
Letters
Article



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Editorial

Top

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.

Correspondence

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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

Climate adaptation in India pp232 - 233
G. Dhanapal
doi:10.1038/nclimate2114

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.

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.

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

Commentaries

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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.

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.

Feature

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Siphoning for safety p240
Bronwyn Wake
doi:10.1038/nclimate2185

Market Watch

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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.

Research Highlights

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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

News and Views

Top

Climate policy: Risk-averse governments pp245 - 246
Paul G. Harris
doi:10.1038/nclimate2176
Relative to the scale of the problem, climate policies worldwide have failed. Now research explains why policy innovations are often inadequate, routinely reflecting the aversion of policymakers to the risk of failure.

Water-energy nexus: Assessing integrated systems pp246 - 247
Mark Howells and H-Holger Rogner
doi:10.1038/nclimate2180
The various supply chains that deliver the services society needs are often managed in silos. Research now shows the advantages of integrated management.

Climate projection: Testing climate assumptions pp248 - 249
David A. Stainforth
doi:10.1038/nclimate2172
Studies often assume that climate is equally sensitive to emissions of warming greenhouse gases and cooling sulphate aerosols. Now, research illustrates that this is not true in models and that without this assumption recent assessments would have produced higher estimates of future temperatures.
See also: Letter by Drew T. Shindell

Oceanography: Southern Ocean polynya pp249 - 250
Arnold L. Gordon
doi:10.1038/nclimate2179
From 1974 to 1976, an unexpected large hole appeared in the Weddell Sea winter sea-ice cover, a consequence of ocean heat carried to the sea surface by convection. This may have been a window to the past, as model analysis suggests anthropogenic climate change will diminish the chances of a repeat performance.
See also: Letter by Casimir de Lavergne et al.

Agricultural Impacts: Robust uncertainty pp251 - 252
Reimund P. Rötter
doi:10.1038/nclimate2181
An up-to-date synthesis of climate change impacts on crop yields shows that the bounds of uncertainty are increasing. So why do estimates of the effect of climate change on crop productivity differ so much?
See also: Letter by A. J. Challinor et al.

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Perspectives

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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.

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.

Letters

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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.

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.

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

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

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.

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

Article

Top

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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