Tuesday, March 26, 2013

Nature Climate Change Contents April 2013 Volume 3 Number 4 pp 303-427

Nature Climate Change

TABLE OF CONTENTS

April 2013 Volume 3, Issue 4

Editorials
Commentary
Market Watch
Research Highlights
News and Views
Perspective
Review
Letters
Articles
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Robust estimation of microbial diversity in theory and in practice
The authors analyse nine metagenomic data sets, and recommend the use of Shannon and Simpson diversity rather than species richness in efforts to quantify and compare microbial diversity.

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Editorials

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Mitigating circumstances p303
doi:10.1038/nclimate1868
There are many barriers that must be overcome if South Africa is to control its greenhouse-gas emissions.

Climate consensus p303
doi:10.1038/nclimate1875
People's acceptance of global warming can be influenced by many filters.

Commentary

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Limits to adaptation pp305 - 307
Kirstin Dow, Frans Berkhout, Benjamin L. Preston, Richard J. T. Klein, Guy Midgley and M. Rebecca Shaw
doi:10.1038/nclimate1847
An actor-centered, risk-based approach to defining limits to social adaptation provides a useful analytic framing for identifying and anticipating these limits and informing debates over society's responses to climate change.

Market Watch

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Power player pp308 - 309
Anna Petherick
doi:10.1038/nclimate1861
South Africa is trying to make its economy greener. But it must work hard to stay on target and tread a fine diplomatic line, writes Anna Petherick.

Research Highlights

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Soil biogeochemistry: Soil microbes find shelter | Water resources: Depleting aquifers | Sea-Ice extent: Arctic marine access | Atmospheric science: Short-term impacts | Policy: Caribbean renewable energy

News and Views

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Expert judgement assessment: Quantifying uncertainty on thin ice pp311 - 312
R. M. Cooke
doi:10.1038/nclimate1860
The contribution of ice sheets to sea-level rise still has large uncertainties that are yet to be quantified.
See also: Article by J. L. Bamber et al.

Psychology: Seeing is believing pp312 - 313
Elke U. Weber
doi:10.1038/nclimate1859
Or do we see something, because we believe it? Evidence suggests that personal experience is more likely to influence Americans with no strong beliefs about climate change than those with firm beliefs.
See also: Letter by Teresa A. Myers et al.

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Perspective

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Global insights into water resources, climate change and governance pp315 - 321
R. Quentin Grafton, Jamie Pittock, Richard Davis, John Williams, Guobin Fu, Michele Warburton, Bradley Udall, Ronnie McKenzie, Xiubo Yu, Nhu Che, Daniel Connell, Qiang Jiang, Tom Kompas, Amanda Lynch, Richard Norris, Hugh Possingham and John Quiggin
doi:10.1038/nclimate1746
The high levels of water extraction from the Colorado, Murray, Orange and Yellow rivers are shown to be the main cause of reduced flows in these systems. Changes in governance are urgently required to preserve the health of these rivers, especially in light of the present and future impacts of climate change.

Review

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Ground water and climate change pp322 - 329
Richard G. Taylor, Bridget Scanlon, Petra Döll, Matt Rodell, Rens van Beek, Yoshihide Wada, Laurent Longuevergne, Marc Leblanc, James S. Famiglietti, Mike Edmunds, Leonard Konikow, Timothy R. Green, Jianyao Chen, Makoto Taniguchi, Marc F. P. Bierkens, Alan MacDonald, Ying Fan, Reed M. Maxwell, Yossi Yechieli, Jason J. Gurdak, Diana M. Allen, Mohammad Shamsudduha, Kevin Hiscock, Pat J.-F. Yeh, Ian Holman and Holger Treidel
doi:10.1038/nclimate1744
Groundwater is of crucial importance for water and food security and for sustaining ecosystems. This Review assesses the likely impacts of climate change on groundwater and groundwater-driven feedbacks to the climate system.

Letters

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Changing social contracts in climate-change adaptation pp330 - 333
W. Neil Adger, Tara Quinn, Irene Lorenzoni, Conor Murphy and John Sweeney
doi:10.1038/nclimate1751
A survey conducted in England and Ireland after a major flooding event shows that perceptions of individual responsibility for protection depend on the specific social and policy context. Perception of future risk, in the case of people directly affected by the flooding, also depends on the context. Expectations about the state’s responsibility for climate protection are critical in promoting longer-term adaptation to the changing climate.

Your opinion on climate change might not be as common as you think pp334 - 337
Z. Leviston, I. Walker and S. Morwinski
doi:10.1038/nclimate1743
Political and media debate on the existence and causes of climate change often rests on claims about what most citizens really think. New research demonstrates that people overestimate how common their own opinion is, and when they do they are less likely to change their view. People also overestimate how many reject the existence of climate change.

Stock dynamics and emission pathways of the global aluminium cycle pp338 - 342
Gang Liu, Colton E. Bangs and Daniel B. Müller
doi:10.1038/nclimate1698
The long-term demand for materials and the opportunities for scrap recycling depend on the stock dynamics of the products in use. In the case of aluminium, research shows that new technologies in primary production can reduce emissions while the aluminium stocks grow, but beyond stock saturation the largest reduction potential shifts to scrap recycling.

The relationship between personal experience and belief in the reality of global warming pp343 - 347
Teresa A. Myers, Edward W. Maibach, Connie Roser-Renouf, Karen Akerlof and Anthony A. Leiserowitz
doi:10.1038/nclimate1754
Research in America finds that observable climate impacts increase people’s certainty about global warming and that prior certainty shapes people’s perceptions of the impacts. The first process happens frequently among people less engaged in the issue of climate change whereas the second process is typical of people already convinced about it.
See also: News and Views by Elke U. Weber

Patterns in household-level engagement with climate change in Indonesia pp348 - 351
Erin L. Bohensky, Alex Smajgl and Tom Brewer
doi:10.1038/nclimate1762
Understanding public engagement with climate change in developing countries is critical for the success of local adaptation strategies. A study in Indonesia shows that nearly one-third of the population has observed and perceived risks of climate change—contrary to previous research suggesting low levels of awareness—but has not taken action to address it.

Global perceptions of local temperature change pp352 - 356
Peter D. Howe, Ezra M. Markowitz, Tien Ming Lee, Chia-Ying Ko and Anthony Leiserowitz
doi:10.1038/nclimate1768
Research based on a survey across 89 countries demonstrates that individuals who live in places with rising average temperatures are more likely than others to perceive local warming. The study also suggests that personal experience of the impacts of climate change may shift public opinion about the reality of global warming.

Assessment of the first consensus prediction on climate change pp357 - 359
David J. Frame and Dáithí A. Stone
doi:10.1038/nclimate1763
In 1990 the First Assessment Report of the Intergovernmental Panel on Climate Change was produced. It contained a prediction of the global-mean-temperature trend for 1990–2030 which, halfway through that period, appears accurate. This is remarkable in hindsight, considering a number of important external forcings were not included. This study concludes the greenhouse-gas-induced warming is largely overwhelming the other forcings.

Spectral biases in tree-ring climate proxies pp360 - 364
Jörg Franke, David Frank, Christoph C. Raible, Jan Esper and Stefan Brönnimann
doi:10.1038/nclimate1816
Seamless quantification of past and present climate variability is needed to understand the Earth’s climate well enough to make accurate predictions for the future. This study addresses whether tree-ring-dominated proxy data properly represent the frequency spectrum of true climate variability. The results challenge the validity of detection and attribution investigations based on these data.

Management of trade-offs in geoengineering through optimal choice of non-uniform radiative forcing pp365 - 368
Douglas G. MacMartin, David W. Keith, Ben Kravitz and Ken Caldeira
doi:10.1038/nclimate1722
This study looks at solar radiation management and how the benefits will vary between regions. Using a general circulation model, the trade-offs between optimizing latitudinal and seasonal distribution of reduced solar radiation are investigated.

Robustness and uncertainties in the new CMIP5 climate model projections pp369 - 373
Reto Knutti and Jan Sedlá?ek
doi:10.1038/nclimate1716
Updated models are being used for the new assessment report from the Intergovernmental Panel on Climate Change. This study compares projections from the latest models with those from earlier versions. The spread of results has not changed significantly, and some of the spread will always remain due to the internal variability of the climate system. As models improve, they are able to represent more processes in greater detail, allowing for greater confidence in their projections, in spite of model spread.

Evidence of the dependence of groundwater resources on extreme rainfall in East Africa pp374 - 378
Richard G. Taylor, Martin C. Todd, Lister Kongola, Louise Maurice, Emmanuel Nahozya, Hosea Sanga and Alan M. MacDonald
doi:10.1038/nclimate1731
Recharge sustains groundwater resources that are depended on globally for drinking water and irrigated agriculture. A newly compiled 55-year record of groundwater-level observations in an aquifer in central Tanzania reveals the highly episodic occurrence of recharge resulting from anomalously intense seasonal rainfall. Model projections show a shift towards more intense monthly rainfall, which favours groundwater recharge, suggesting it may be a viable adaptation water source in the future.

Response of snow-dependent hydrologic extremes to continued global warming pp379 - 384
Noah S. Diffenbaugh, Martin Scherer and Moetasim Ashfaq
doi:10.1038/nclimate1732
Snow accumulation is critical for water availability in the Northern Hemisphere. Model projections show a shift towards low snow years, with areas of western North America, northeastern Europe and the Greater Himalayas showing the strongest decline. Many snow-dependent regions are likely to experience increasing stress from low snow years if global warming exceeds 2° above the pre-industrial baseline.

The impact of global land-cover change on the terrestrial water cycle pp385 - 390
Shannon M. Sterling, Agnès Ducharne and Jan Polcher
doi:10.1038/nclimate1690
Human impacts on the terrestrial water cycle have the potential to influence hazards such as flooding and drought, so understanding the extent of our influence is an important research goal. A study utilizing estimates of evapotranspiration for different types of land cover and a database of changes in use now shows that the extent of land-cover change caused by people is already an important factor affecting the terrestrial water cycle.

Catchment productivity controls CO2 emissions from lakes pp391 - 394
Stephen C. Maberly, Philip A. Barker, Andy W. Stott and Mitzi M. De Ville
doi:10.1038/nclimate1748
Most lakes are net sources of CO2; conventionally the CO2 in lake waters is attributed to in-lake oxidation of terrestrially-produced dissolved organic carbon. Now research indicates that CO2 in lakes may be delivered directly via inflowing streams. These findings suggest that future CO2 emissions from lakes will be strongly related to productivity in the lake catchment.

The temperature response of soil microbial efficiency and its feedback to climate pp395 - 398
Serita D. Frey, Juhwan Lee, Jerry M. Melillo and Johan Six
doi:10.1038/nclimate1796
Soils are the largest repository of organic carbon in the terrestrial biosphere. Nevertheless, relatively little is known about the factors controlling the efficiency with which microbial communities utilize carbon, and its effect on soil–atmosphere CO2 exchange. Now research using long-term experimental plots suggests that climate warming could alter the decay dynamics of more stable organic-matter compounds with implications for carbon storage in soils and ultimately climate warming.

Articles

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The pivotal role of perceived scientific consensus in acceptance of science pp399 - 404
Stephan Lewandowsky, Gilles E. Gignac and Samuel Vaughan
doi:10.1038/nclimate1720
Public concern about anthropogenic global warming has been declining despite the scientific consensus on the issue. It is still unknown whether experts’ consensus determines people’s beliefs, and it is not clear if public perception of consensus overrides worldviews known to foster rejection of anthropogenic climate change. New research shows that information about scientific consensus increases acceptance of anthropogenic global warming and neutralizes the effect of worldviews.

2020 emissions levels required to limit warming to below 2 °C pp405 - 412
Joeri Rogelj, David L. McCollum, Brian C. O’Neill and Keywan Riahi
doi:10.1038/nclimate1758
A relatively wide range of emissions in 2020 could keep open the option of limiting long-term temperature increase to below 2 °C; however, a shortfall in critical technologies would narrow that range or eliminate it altogether. Reduced emissions in 2020 would hedge against this uncertainty.

Comparing the effectiveness of monetary versus moral motives in environmental campaigning pp413 - 416
J. W. Bolderdijk, L. Steg, E. S. Geller, P. K. Lehman and T. Postmes
doi:10.1038/nclimate1767
Environmental campaigns often promote energy conservation by appealing to economic rather than environmental concerns, assuming self-interest drives people’s behaviour. New research discredits such conventional wisdom and shows that, at least in some cases, it is more effective to call on people’s interest in protecting the biosphere to encourage behavioural changes.

Changes in South Pacific rainfall bands in a warming climate pp417 - 423
Matthew J. Widlansky, Axel Timmermann, Karl Stein, Shayne McGregor, Niklas Schneider, Matthew H. England, Matthieu Lengaigne and Wenju Cai
doi:10.1038/nclimate1726
The South Pacific Convergence Zone is the largest rainband in the Southern Hemisphere, and its response to global warming is still undetermined. In this study a hierarchy of climate models show that the uncertainty in rainfall projections in the South Pacific Convergence Zone is the result of two competing mechanisms.

An expert judgement assessment of future sea level rise from the ice sheets pp424 - 427
J. L. Bamber and W. P. Aspinall
doi:10.1038/nclimate1778
This study uses a formalized pooling of expert views on uncertainties in the future contributions of melting ice sheets to sea-level rise, using a structured elicitation approach. The median estimate obtained is substantially larger than that found by previous studies. Expert opinion is shown to be both very uncertain and undecided on the key issue of whether recent ice-sheet behaviour is a long-term trend or due to natural variability.
See also: News and Views by R. M. Cooke

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