Thursday, August 25, 2016

Nature Climate Change Contents: September 2016 Volume 6 Number 9 pp 803-890

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TABLE OF CONTENTS

September 2016 Volume 6, Issue 9

Editorial
Correspondence
Commentaries
Correction
News Feature
Research Highlights
News and Views
Perspective
Review
Letters
Articles
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Editorial

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Global reach and engagement p803
doi:10.1038/nclimate3120
Popular culture reflects both the interests of and the issues affecting the general public. As concerns regarding climate change and its impacts grow, is it permeating into popular culture and reaching that global audience?

Correspondence

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Policy institutions and forest carbon p805
Annette Cowie, Fabiano Ximenes, Göran Berndes, Miguel Brandão, Patrick Lamers and Gregg Marland
doi:10.1038/nclimate3093

Reply to 'Policy institutions and forest carbon' pp805 - 806
Andrew Macintosh, Heather Keith and David Lindenmayer
doi:10.1038/nclimate3094

Commentaries

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El Niño and a record CO2 rise pp806 - 810
Richard A. Betts, Chris D. Jones, Jeff R. Knight, Ralph F. Keeling and John J. Kennedy
doi:10.1038/nclimate3063
The recent El Niño event has elevated the rise in CO2 concentration this year. Here, using emissions, sea surface temperature data and a climate model, we forecast that the CO2 concentration at Mauna Loa will for the first time remain above 400 ppm all year, and hence for our lifetimes.

Earth's surface water change over the past 30 years pp810 - 813
Gennadii Donchyts, Fedor Baart, Hessel Winsemius, Noel Gorelick, Jaap Kwadijk and Nick van de Giesen
doi:10.1038/nclimate3111
Earth's surface gained 115,000 km2 of water and 173,000 km2 of land over the past 30 years, including 20,135 km2 of water and 33,700 km2 of land in coastal areas. Here, we analyse the gains and losses through the Deltares Aqua Monitor — an open tool that detects land and water changes around the globe.

The attribution question pp813 - 816
Friederike E. L. Otto, Geert Jan van Oldenborgh, Jonathan Eden, Peter A. Stott, David J. Karoly and Myles R. Allen
doi:10.1038/nclimate3089
Understanding how the overall risks of extreme events are changing in a warming world requires both a thermodynamic perspective and an understanding of changes in the atmospheric circulation.

Correction

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Correction p816
doi:10.1038/nclimate3102

News Feature

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Contested territory pp817 - 820
Michael Green
doi:10.1038/nclimate3112
Some Pacific Island communities are already moving themselves beyond rising tides, but there's nothing simple about how, why or when they're doing it.

Research Highlights

Top

Biodiversity: Double whammy | Attribution: Heatwave mortality | Climate communication: Uncertain reporting | Cryospheric science: Glaciers status

News and Views

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Climate response: Strong warming at high emissions pp823 - 824
Thomas L. Frölicher
doi:10.1038/nclimate3053
The ratio of global temperature change to cumulative emissions is relatively constant up to two trillion tonnes of carbon emissions. Now a new modelling study suggests that the concept of a constant ratio is even applicable to higher cumulative carbon emissions, with important implications for future warming.
See also: Letter by Katarzyna B. Tokarska et al.

Atmospheric dynamics: Arctic winds of change pp824 - 825
Dirk Notz
doi:10.1038/nclimate3030
The Earth's climate evolves in response to both externally forced changes and internal variability. Now research suggests that both drivers combine to set the pace of Arctic warming caused by large-scale sea-ice loss.
See also: Letter by James A. Screen et al.

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Perspective

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Science and policy characteristics of the Paris Agreement temperature goal pp827 - 835
Carl-Friedrich Schleussner, Joeri Rogelj, Michiel Schaeffer, Tabea Lissner, Rachel Licker, Erich M. Fischer, Reto Knutti, Anders Levermann, Katja Frieler and William Hare
doi:10.1038/nclimate3096
There are discernible differences in climate impacts between 1.5 °C and 2 °C of warming. The extent of countries' near-term mitigation ambition will determine the success of the Paris Agreement's temperature goal.

Review

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Key ecological responses to nitrogen are altered by climate change pp836 - 843
T. L. Greaver, C. M. Clark, J. E. Compton, D. Vallano, A. F. Talhelm, C. P. Weaver, L. E. Band, J. S. Baron, E. A. Davidson, C. L. Tague, E. Felker-Quinn, J. A. Lynch, J. D. Herrick, L. Liu, C. L. Goodale, K. J. Novak and R. A. Haeuber
doi:10.1038/nclimate3088
In this Review the cumulative effects of anthropogenic nitrogen and climate change are considered. Including how climate alters nitrogen cycling and availability, and the impact of nitrogen addition on carbon cycling, acidification and biodiversity.

Letters

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Economic gains stimulate negative evaluations of corporate sustainability initiatives pp844 - 846
Tamar Makov and George E. Newman
doi:10.1038/nclimate3033
Businesses are increasingly undertaking initiatives that increase profit and provide environmental benefits. They risk backlash, however, as people are shown to respond negatively to the notion of a business profiting from such initiatives.

Mental representation changes the evaluation of green product benefits pp847 - 850
Kelly Goldsmith, George E. Newman and Ravi Dhar
doi:10.1038/nclimate3019
Many campaigns to get people to purchase sustainable products highlight self-interest. However, experiments now show that emphasizing the environmental benefit of such goods may be more effective.

The climate response to five trillion tonnes of carbon pp851 - 855
Katarzyna B. Tokarska, Nathan P. Gillett, Andrew J. Weaver, Vivek K. Arora and Michael Eby
doi:10.1038/nclimate3036
Long-term model simulations show that a linear relationship between atmospheric warming and cumulative CO2 emissions holds up to 5 trillion tonnes of carbon (EgC), the estimated total fossil fuel resource in the absence of mitigation efforts.
See also: News and Views by Thomas L. Frölicher

Contribution of sea-ice loss to Arctic amplification is regulated by Pacific Ocean decadal variability pp856 - 860
James A. Screen and Jennifer A. Francis
doi:10.1038/nclimate3011
This study suggests that the Pacific Decadal Oscillation phase influences how much sea-ice loss contributes to Arctic amplification, with warming being larger during the negative phase with greater sea-ice loss.
See also: News and Views by Dirk Notz

Detecting failure of climate predictions pp861 - 864
Michael C. Runge, Julienne C. Stroeve, Andrew P. Barrett and Eve McDonald-Madden
doi:10.1038/nclimate3041
This study shows how failure to capture system dynamics can be detected in climate model predictions. This information should improve model projections and facilitate better decision-making.

Longer growing seasons shift grassland vegetation towards more-productive species pp865 - 868
Jason D. Fridley, Josh S. Lynn, J. P. Grime and A. P. Askew
doi:10.1038/nclimate3032
A 20-year grassland experiment shows links between plant functional traits and the climate. Species favoured by extended growing seasons have taller canopies and faster assimilation rates, at the expense of those with high leaf-tissue investment.

Land–atmosphere feedbacks amplify aridity increase over land under global warming pp869 - 874
Alexis Berg, Kirsten Findell, Benjamin Lintner, Alessandra Giannini, Sonia I. Seneviratne, Bart van den Hurk, Ruth Lorenz, Andy Pitman, Stefan Hagemann, Arndt Meier, Frédérique Cheruy, Agnès Ducharne, Sergey Malyshev and P. C. D. Milly
doi:10.1038/nclimate3029
Aridity is expected to increase globally in a warmer world. Research now suggests that this is substantially amplified by land–atmosphere feedbacks associated with the land surface’s response to climate and plant responses to increased atmospheric CO2.

Drought rewires the cores of food webs pp875 - 878
Xueke Lu, Clare Gray, Lee E. Brown, Mark E. Ledger, Alexander M. Milner, Raúl J. Mondragón, Guy Woodward and Athen Ma
doi:10.1038/nclimate3002
Droughts are intensifying under climate change. Research into the resilience of stream food webs to drought now shows that ‘rewiring’ of food web structure in the face of species losses helps to buffer changes to the overall network structure.

Articles

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Social norms and efficacy beliefs drive the Alarmed segment’s public-sphere climate actions pp879 - 884
Kathryn L. Doherty and Thomas N. Webler
doi:10.1038/nclimate3025
The people that are most concerned about climate change do not always take action. Behavioural modelling shows that concerned citizens are more likely to act if they believe similar people are taking action, and that their action will make a difference.

Climate change impact modelling needs to include cross-sectoral interactions pp885 - 890
Paula A. Harrison, Robert W. Dunford, Ian P. Holman and Mark D. A. Rounsevell
doi:10.1038/nclimate3039
A model comparison shows that integrated and sector-specific models suggest different results for various climate impacts. The discrepancies are particularly pronounced for indicators such as food production and water exploitation.

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