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Nature Climate Change Contents: March 2016 Volume 6 Number 3 pp 219-323

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TABLE OF CONTENTS

March 2016 Volume 6, Issue 3

Editorials
Correspondence
Commentaries
Research Highlights
News and Views
Perspectives
Letters
Articles
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Nature Geoscience Focus on Groundwater 

In this focus, we present a collection of research papers and opinion pieces that discuss the influence of groundwater on hydrological, environmental and geological processes.

Read the article, The global volume and distribution of modern groundwaterfree to registered users until the 2 March 2016.



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Nature Geoscience Focus on Groundwater 

In this focus, we present a collection of research papers and opinion pieces that discuss the influence of groundwater on hydrological, environmental and geological processes.

Read the article, The global volume and distribution of modern groundwater, free to registered users until the 2 March 2016.
 
 

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Editorials

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Reading science p219
doi:10.1038/nclimate2953
Scientists are often accused of poorly communicating their findings, but improving scientific literacy is everyone's responsibility.

Topping the tables p219
doi:10.1038/nclimate2955
Failure of climate change mitigation and adaptation ranks as the most impactful risk to society, according to the 2016 Global Risks Report from the World Economic Forum.

Correspondence

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Greenhouse gas emissions from synthetic natural gas production pp220 - 221
Sheng Li and Lin Gao
doi:10.1038/nclimate2887
See also: Correspondence by Chi-Jen Yang et al.

Reply to 'Greenhouse gas emissions from synthetic natural gas production' pp221 - 222
Chi-Jen Yang and Robert B. Jackson
doi:10.1038/nclimate2889
See also: Correspondence by Sheng Li et al.

Commentaries

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1.5 °C and climate research after the Paris Agreement pp222 - 224
Mike Hulme
doi:10.1038/nclimate2939
The Paris Agreement contains an ambition to limit global warming to no more than 1.5 °C above pre-industrial levels, changing the context for policy-relevant research and extending a challenge to the IPCC and researchers.

Making sense of the early-2000s warming slowdown pp224 - 228
John C. Fyfe, Gerald A. Meehl, Matthew H. England, Michael E. Mann, Benjamin D. Santer, Gregory M. Flato, Ed Hawkins, Nathan P. Gillett, Shang-Ping Xie, Yu Kosaka and Neil C. Swart
doi:10.1038/nclimate2938
It has been claimed that the early-2000s global warming slowdown or hiatus, characterized by a reduced rate of global surface warming, has been overstated, lacks sound scientific basis, or is unsupported by observations. The evidence presented here contradicts these claims.

Keeping the lights on for global ocean salinity observation pp228 - 231
Paul J. Durack, Tong Lee, Nadya T. Vinogradova and Detlef Stammer
doi:10.1038/nclimate2946
Insights about climate are being uncovered thanks to improved capacities to observe ocean salinity, an essential climate variable. However, cracks are beginning to appear in the ocean observing system that require prompt attention if we are to maintain the existing, hard-won capacity into the near future.

Research Highlights

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Hydrology: Amazon flooding | Energy modelling: Environmental impact | Geoengineering: Ship wake brightening | Precipitation: Recent US trends

News and Views

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Ocean–atmosphere dynamics: Atlantic origin of Pacific changes pp233 - 234
Shayne McGregor
doi:10.1038/nclimate2866
Unprecedented strengthening of Pacific trade winds has occurred in recent decades, while both the Indian and Atlantic Ocean surface temperatures warmed. Now a study suggests that the Atlantic Ocean warming is driving this Pacific trade wind strengthening and the warming of the Indian Ocean.
See also: Letter by Xichen Li et al.

Arctic warming: Short-term solutions pp234 - 235
Julia Schmale
doi:10.1038/nclimate2897
Arctic temperatures are increasing because of long- and short-lived climate forcers, with reduction of the short-lived species potentially offering some quick mitigation. Now a regional assessment reveals the emission locations of these short-lived species and indicates international co-operation is needed to develop an effective mitigation plan.
See also: Letter by M. Sand et al.

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Perspectives

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Wealth reallocation and sustainability under climate change pp237 - 244
Eli P. Fenichel, Simon A. Levin, Bonnie McCay, Kevin St. Martin, Joshua K. Abbott and Malin L. Pinsky
doi:10.1038/nclimate2871
This Perspective links climate change and the distribution of wealth. Using an 'inclusive wealth' framework, it is shown that climate change could dramatically reallocate wealth, with important implications for sustainable development.

Differences between carbon budget estimates unravelled pp245 - 252
Joeri Rogelj, Michiel Schaeffer, Pierre Friedlingstein, Nathan P. Gillett, Detlef P. van Vuuren, Keywan Riahi, Myles Allen and Reto Knutti
doi:10.1038/nclimate2868
Estimates of carbon budgets compatible with limiting warming to below specific temperature limits are reviewed, and reasons underlying their differences discussed along with their respective strengths and limitations.

Overestimation of marsh vulnerability to sea level rise pp253 - 260
Matthew L. Kirwan, Stijn Temmerman, Emily E. Skeehan, Glenn R. Guntenspergen and Sergio Fagherazzi
doi:10.1038/nclimate2909
In this Perspective it is argued that coastal marsh vulnerability is often overstated because assessments generally neglect feedback processes known to accelerate soil building with sea level rise, as well as the potential for marshes to migrate inland.

Letters

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National-level progress on adaptation pp261 - 264
Alexandra Lesnikowski, James Ford, Robbert Biesbroek, Lea Berrang-Ford and S. Jody Heymann
doi:10.1038/nclimate2863
Rigorous measurement of adaptation policies is crucial to implementing successful climate policy. Policy analysis of 41 countries shows an 87% increase in adaptation initiatives since 2010, suggesting that concrete adoption of such practices is growing.

Strategic reasoning and bargaining in catastrophic climate change games pp265 - 268
Vilhelm Verendel, Daniel J. A. Johansson and Kristian Lindgren
doi:10.1038/nclimate2849
A game theory experiment shows that it is easier to reach an agreement to avert the worst impacts of climate change when a catastrophic threshold is known. It also shows that countries’ use of strategic reasoning puts such agreements at risk.

An increase in aerosol burden and radiative effects in a warmer world pp269 - 274
Robert J. Allen, William Landuyt and Steven T. Rumbold
doi:10.1038/nclimate2827
Modelling allows estimation of aerosol–climate feedbacks on the Earth’s radiative balance and suggests that climate change may increase aerosol burden and surface concentration, negatively affecting future air quality.

Atlantic-induced pan-tropical climate change over the past three decades pp275 - 279
Xichen Li, Shang-Ping Xie, Sarah T. Gille and Changhyun Yoo
doi:10.1038/nclimate2840
The dipole-like trend of tropical sea surface temperature is investigated and this study finds it to be initiated in the Atlantic Ocean. Atlantic warming drives wind and circulation changes and influences Pacific Ocean surface temperatures.
See also: News and Views by Shayne McGregor

Mapping the future expansion of Arctic open water pp280 - 285
Katherine R. Barnhart, Christopher R. Miller, Irina Overeem and Jennifer E. Kay
doi:10.1038/nclimate2848
This study uses model projections of the open water season (for 1920–2100) to investigate Arctic sea-ice decline. Nearshore regions began shifting from pre-industrial conditions in 1990, and human influence is projected to emerge in 2040.

Response of Arctic temperature to changes in emissions of short-lived climate forcers pp286 - 289
M. Sand, T. K. Berntsen, K. von Salzen, M. G. Flanner, J. Langner and D. G. Victor
doi:10.1038/nclimate2880
Arctic temperatures are most sensitive to emissions of short-lived climate forcers from a small number of Arctic nations (Russia and Nordic countries) that are also the most impacted by this warming, easing the implementation of mitigation strategies.
See also: News and Views by Julia Schmale

Impact of solar panels on global climate pp290 - 294
Aixue Hu, Samuel Levis, Gerald A. Meehl, Weiqing Han, Warren M. Washington, Keith W. Oleson, Bas J. van Ruijven, Mingqiong He and Warren G. Strand
doi:10.1038/nclimate2843
This study considers how large-scale application of solar panels will affect climate. Electricity generation leads to regional cooling but this is countered by the power’s use, affecting global circulation patterns with changes in regional rainfall.

Multi-scale predictions of massive conifer mortality due to chronic temperature rise pp295 - 300
N. G. McDowell, A. P. Williams, C. Xu, W. T. Pockman, L. T. Dickman, S. Sevanto, R. Pangle, J. Limousin, J. Plaut, D. S. Mackay, J. Ogee, J. C. Domec, C. D. Allen, R. A. Fisher, X. Jiang, J. D. Muss, D. D. Breshears, S. A. Rauscher and C. Koven
doi:10.1038/nclimate2873
Research integrating experimental data and modelling to improve representation of plant physiological thresholds infers largely temperature-driven loss of conifer trees by 2100 across the southwestern USA and much of the Northern Hemisphere.

Designer policy for carbon and biodiversity co-benefits under global change pp301 - 305
Brett A. Bryan, Rebecca K. Runting, Tim Capon, Michael P. Perring, Shaun C. Cunningham, Marit E. Kragt, Martin Nolan, Elizabeth A. Law, Anna R. Renwick, Sue Eber, Rochelle Christian and Kerrie A. Wilson
doi:10.1038/nclimate2874
Carbon payments for afforestation can help mitigate climate change and declining biodiversity. This paper evaluates 14 policy mechanisms for supplying carbon and biodiversity benefits through reforestation in Australia’s 85.3 Mha of agricultural land.

Large divergence of satellite and Earth system model estimates of global terrestrial CO2 fertilization pp306 - 310
W. Kolby Smith, Sasha C. Reed, Cory C. Cleveland, Ashley P. Ballantyne, William R. L. Anderegg, William R. Wieder, Yi Y. Liu and Steven W. Running
doi:10.1038/nclimate2879
Satellite-derived estimates of increases in terrestrial net primary productivity are less than half of those derived from Earth system models. This discrepancy is explained by over-sensitivity of Earth system models to atmospheric CO2 concentrations.

Articles

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Linguistic analysis of IPCC summaries for policymakers and associated coverage pp311 - 316
Ralf Barkemeyer, Suraje Dessai, Beatriz Monge-Sanz, Barbara Gabriella Renzi and Giulio Napolitano
doi:10.1038/nclimate2824
The IPCC summaries written for policymakers are meant to communicate findings to a wide audience. Textual analysis shows that these reports continue to have low readability, in contrast with media coverage.

Cooling of US Midwest summer temperature extremes from cropland intensification pp317 - 322
Nathaniel D. Mueller, Ethan E. Butler, Karen A. McKinnon, Andrew Rhines, Martin Tingley, N. Michele Holbrook and Peter Huybers
doi:10.1038/nclimate2825
Increases in temperature extremes are of major concern for agricultural production. However, this study identifies a connection between agricultural intensification and less extreme summer temperatures over the agriculturally dominated US Midwest.

Revaluating ocean warming impacts on global phytoplankton pp323 - 330
Michael J. Behrenfeld, Robert T. O’Malley, Emmanuel S. Boss, Toby K. Westberry, Jason R. Graff, Kimberly H. Halsey, Allen J. Milligan, David A. Siegel and Matthew B. Brown
doi:10.1038/nclimate2838
Satellite measurements of chlorophyll are used to infer phytoplankton biomass changes and the relationship to sea surface temperature. This study shows that chlorophyll changes can be light-driven so the temperature–biomass relationship may not hold in the future.

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