Friday, May 25, 2012

Nature Climate Change Contents June 2012 Volume 2 Number 6 pp 375-468

Nature Chemistry
TABLE OF CONTENTS

June 2012 Volume 2, Issue 6

In This Issue
Editorial
Correspondence
Commentaries
News Feature
Corrections
Policy Watch
Research Highlights
News and Views
Perspective
Review
Letters
Article
Beyond Boundaries

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In This Issue

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In this issue
doi:10.1038/nclimate1563
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Editorial

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Brazil takes centre stage p375
doi:10.1038/nclimate1574
Brazil's hosting of the much anticipated Rio+20 United Nations Conference on Sustainable Development this month will put the country in the climate change spotlight.
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Correspondence

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Managing exposure to flooding in New York City p377
Jeroen C. J. H. Aerts and W. J. Wouter Botzen
doi:10.1038/nclimate1487
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See also: Article by Ning Lin et al.

Assessing climate risks to UK agriculture p378
Jerry W. Knox and Steven Wade
doi:10.1038/nclimate1538
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See also: Commentary by Mikhail A. Semenov et al.

Commentaries

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Rio+20 and Brazil's policy on climate change pp379 - 380
Eduardo Fernandez Silva
doi:10.1038/nclimate1525
As host to the Rio+20 United Nations Conference on Sustainable Development, Brazil will draw international attention to its policy on climate change, but the measures announced so far are not commensurate with the recently set reduction goal.
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Shortcomings in wheat yield predictions pp380 - 382
Mikhail A. Semenov, Rowan A. C. Mitchell, Andrew P. Whitmore, Malcolm J. Hawkesford, Martin A. J. Parry and Peter R. Shewry
doi:10.1038/nclimate1511
Predictions of a 40–140% increase in wheat yield by 2050, reported in the UK Climate Change Risk Assessment, are based on a simplistic approach that ignores key factors affecting yields and hence are seriously misleading.
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See also: Correspondence by Jerry W. Knox et al.

Greenhouse-gas emissions from tropical dams pp382 - 384
Philip M. Fearnside and Salvador Pueyo
doi:10.1038/nclimate1540
Emissions from tropical hydropower are often underestimated and can exceed those of fossil fuel for decades.
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Shale gas can be a double-edged sword for climate change pp385 - 387
Deyi Hou, Jian Luo and Abir Al-Tabbaa
doi:10.1038/nclimate1500
Shale gas can be a powerful tool in combating climate change. However, its exploitation may also lead to undesired environmental effects that can conversely worsen climate change.
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News Feature

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Waste not want not pp388 - 391
Sonja van Renssen
doi:10.1038/nclimate1541
Industrial symbiosis — the sharing of by-product resources among diverse industries — can reduce costs and improve the environment. But despite its benefits, it is no panacea.
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Corrections

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Correction: Cooking up fuel p391
doi:10.1038/nclimate1543
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Correction: Seeing carbon emissions p391
doi:10.1038/nclimate1545
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Correction: Robustness of warming attribution p402
doi:10.1038/nclimate1549
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Correction: Mapping vulnerabilities p468
doi:10.1038/nclimate1579
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Policy Watch

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Saving EU climate policy pp392 - 393
Sonja van Renssen
doi:10.1038/nclimate1561
Market-based mechanisms to tackle climate change have many advocates, but economic conditions are making emissions trading schemes hard to implement and sustain, explains Sonja van Renssen.
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Research Highlights

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Energy economics: Biofuel economic potential | Modelling: Climate and Baltic Sea nutrients | Technology: Mitigation costs | Scenario analysis: Urbanization emissions | Permafrost: Accounting for snow types | Politics: Voting for climate | Cryoscience: Glacier speeds | Carbon cycle: Certainty about uncertainty | Phenology: Experiments in context

News and Views

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Glaciology: Future of the Greenland ice sheet pp396 - 397
Gerhard Krinner and Gaël Durand
doi:10.1038/nclimate1557
Ice-sheet loss is a likely effect of human interference with the climate system. Research shows that the disintegration of the Greenland ice sheet could occur close to, or even below, the target of limiting warming to 2 °C above pre-industrial levels.
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See also: Letter by Alexander Robinson et al.

Oceanography: Future impact of today's choices pp397 - 398
Ronald J. Stouffer
doi:10.1038/nclimate1550
Climate change is now occurring, but few people consider how long the effects may last. A study emphasizes the long-term climate effects of present-day emissions.
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Energy: Analysing fossil-fuel displacement pp398 - 399
Andrew K. Jorgenson
doi:10.1038/nclimate1552
It is commonly assumed that fossil fuels can be replaced by alternative forms of energy. Now research challenges this assumption, and highlights the role of non-technological solutions to reduce fossil-fuel consumption.
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See also: Letter by Richard York

Migration: The drivers of human migration pp400 - 401
Etienne Piguet
doi:10.1038/nclimate1559
Warnings about torrents of forced migrations owing to climate change make headlines. Now research shows that this is an oversimplification.
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See also: Letter by Dominic R. Kniveton et al.

Migration: Flooding and the scale of migration pp401 - 402
Allan M. Findlay
doi:10.1038/nclimate1554
Immobility rather than mobility should be the focus of concern for policymakers worried about the impact of climate-related natural hazards on the livelihoods of rural populations.
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Perspective

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Quantifying future climate change pp403 - 409
Matthew Collins, Richard E. Chandler, Peter M. Cox, John M. Huthnance, Jonathan Rougier and David B. Stephenson
doi:10.1038/nclimate1414
This Perspective describes techniques for quantifying uncertainties in climate projections in terms of a common framework, whereby models are used to explore relationships between past climate and climate change and future projections.
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Review

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Global agriculture and nitrous oxide emissions pp410 - 416
Dave S. Reay, Eric A. Davidson, Keith A. Smith, Pete Smith, Jerry M. Melillo, Frank Dentener and Paul J. Crutzen
doi:10.1038/nclimate1458
This Review discusses current knowledge regarding agriculture as a source for nitrous oxide — a major greenhouse gas. It offers an outlook on future developments about the consequences of increasing use of biofuels and the potential importance of aquaculture, as well as options for mitigation.
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Evaluation of climate models using palaeoclimatic data pp417 - 424
Pascale Braconnot, Sandy P. Harrison, Masa Kageyama, Patrick J. Bartlein, Valerie Masson-Delmotte, Ayako Abe-Ouchi, Bette Otto-Bliesner and Yan Zhao
doi:10.1038/nclimate1456
This Review focuses on the work of the Palaeoclimate Modelling Intercomparison Project, showing the contribution that palaeoclimate records can make to understanding contemporary climate change by providing a means to test climate models.
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Letters

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135 years of global ocean warming between the Challenger expedition and the Argo Programme pp425 - 428
Dean Roemmich, W. John Gould and John Gilson
doi:10.1038/nclimate1461
Comparison of global-scale measurements of subsurface ocean temperature taken during the epic voyage of HMS Challenger (1872–1876) with data collected by the Argo Programme over the past eight years shows that oceans have been warming at least since the late-nineteenth/early-twentieth century.
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Multistability and critical thresholds of the Greenland ice sheet pp429 - 432
Alexander Robinson, Reinhard Calov and Andrey Ganopolski
doi:10.1038/nclimate1449
A comprehensive stability analysis shows that the critical global temperature rise that leads to collapse of the Greenland ice sheet is only 1–2 °C above the pre-industrial climate state, which is significantly lower than previously believed.
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See also: News and Views by Gerhard Krinner et al.

Overestimation of Mediterranean summer temperature projections due to model deficiencies pp433 - 436
Fredrik Boberg and Jens H. Christensen
doi:10.1038/nclimate1454
This study addresses the importance of systematic biases in regional and global climate models. Simulations for the central Mediterranean region show that, unless a bias-correction method is applied, individual models significantly overestimate regional amplification of global warming.
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Black-carbon reduction of snow albedo pp437 - 440
Odelle L. Hadley and Thomas W. Kirchstetter
doi:10.1038/nclimate1433
This paper reports results from a laboratory experiment designed to quantify the reduction of snow albedo by black carbon. The study aims to test models of radiative transfer in snow and the parameterizations from them that are used in climate models.
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Do alternative energy sources displace fossil fuels? pp441 - 443
Richard York
doi:10.1038/nclimate1451
Analysts implicitily assume that increasing renewable-energy generation by one unit displaces conventional energy by the same amount. Research now shows that, owing to the complexity of our socio–economic systems, each unit of total national non-fossil-fuel energy use displaced less than one-quarter of a unit of fossil-fuel energy use over the past 50 years.
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See also: News and Views by Andrew K. Jorgenson

Emerging migration flows in a changing climate in dryland Africa pp444 - 447
Dominic R. Kniveton, Christopher D. Smith and Richard Black
doi:10.1038/nclimate1447
Despite 20 years of concern about human migration in response to environmental pressure, estimates of the numbers likely to move as a result of climate change remain, at best, guesswork. Now computer simulations reveal complex interactions in the way that climate and demographic changes combine to influence migration, suggesting that we should expect some surprises.
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See also: News and Views by Etienne Piguet

Vulnerability of cloud forest reserves in Mexico to climate change pp448 - 452
Rocío Ponce-Reyes, Víctor-Hugo Reynoso-Rosales, James E. M. Watson, Jeremy VanDerWal, Richard A. Fuller, Robert L. Pressey and Hugh P. Possingham
doi:10.1038/nclimate1453
How effective are protected areas for conserving biodiversity in a rapidly changing world? A study shows that the network of protected areas in Mexico’s cloud forests—a biome with high species richness and a large fraction of endemics—is almost completely redundant in a changing climate.
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Plot-scale evidence of tundra vegetation change and links to recent summer warming pp453 - 457
Sarah C. Elmendorf, Gregory H. R. Henry, Robert D. Hollister, Robert G. Björk, Noémie Boulanger-Lapointe, Elisabeth J. Cooper, Johannes H. C. Cornelissen, Thomas A. Day, Ellen Dorrepaal, Tatiana G. Elumeeva, Mike Gill, William A. Gould, John Harte, David S. Hik, Annika Hofgaard, David R. Johnson, Jill F. Johnstone, Ingibjörg Svala Jónsdóttir, Janet C. Jorgenson, Kari Klanderud, Julia A. Klein, Saewan Koh, Gaku Kudo, Mark Lara, Esther Lévesque, Borgthor Magnússon, Jeremy L. May, Joel A. Mercado-D?´az, Anders Michelsen, Ulf Molau, Isla H. Myers-Smith, Steven F. Oberbauer, Vladimir G. Onipchenko, Christian Rixen, Niels Martin Schmidt, Gaius R. Shaver, Marko J. Spasojevic, Þóra Ellen Þórhallsdóttir, Anne Tolvanen, Tiffany Troxler, Craig E. Tweedie, Sandra Villareal, Carl-Henrik Wahren, Xanthe Walker, Patrick J. Webber, Jeffrey M. Welker and Sonja Wipf
doi:10.1038/nclimate1465
Satellite data suggest that contemporary climate warming has already resulted in increased productivity and shrub biomass over much of the Arctic, but plot-level evidence for vegetation transformation remains sparse. Now research provides plot-scale evidence linking changes in vascular plant abundance to local summer warming in widely dispersed tundra locations across the globe.
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Biogeochemical and ecological feedbacks in grassland responses to warming pp458 - 461
Zhuoting Wu, Paul Dijkstra, George W. Koch and Bruce A. Hungate
doi:10.1038/nclimate1486
Feedbacks can modulate the way plants respond to warming, but difficulties in detecting long-acting feedbacks complicate understanding of the climatic effects on community structure and function beyond initial responses. Now a mesocosm experiment shows that although warming initially increased aboveground net primary productivity in grassland ecosystems, the response diminished progressively over time.
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Article

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Physically based assessment of hurricane surge threat under climate change pp462 - 467
Ning Lin, Kerry Emanuel, Michael Oppenheimer and Erik Vanmarcke
doi:10.1038/nclimate1389
Focusing on New York City, this study investigates the impact of climate change on hurricane storm surges. The analysis shows that the frequency of surge-flooding events is likely to increase greatly owing to the combined effects of storm-climatology change and sea-level rise.
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See also: Correspondence by Jeroen C. J. H. Aerts et al.

Beyond Boundaries

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Integrating knowledge p468
doi:10.1038/nclimate1551
Environmental social scientist Lindsay C. Stringer worked with ecologists, soil and climate scientists, economists, and livelihood and policy experts to examine carbon storage, livelihoods and ecosystem services in subSaharan Africa's drylands.
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