Wednesday, September 25, 2013

Nature Climate Change Contents October 2013 Volume 3 Number 10 pp 849-938

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TABLE OF CONTENTS

October 2013 Volume 3, Issue 10

Editorial
Commentaries
News Feature
Market Watch
Research Highlights
News and Views
Perspective
Review
Letters
Articles
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Editorial

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Campaign Climate p849
doi:10.1038/nclimate2023
A well-organized global grassroots campaign for climate protection could eclipse the IPPC in political influence.

Commentaries

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Climate protection can learn from the AIDS movement pp850 - 851
Jeremy Brecher and Kevin Fisher
doi:10.1038/nclimate1986
Climate protection advocacy can learn from the success of the International AIDS Conference in forging a powerful global movement of scientists, non-governmental organizations and civil society.

China's synthetic natural gas revolution pp852 - 854
Chi-Jen Yang and Robert B. Jackson
doi:10.1038/nclimate1988
China has recently pushed for investments in large-scale coal-fuelled synthetic natural gas plants. The associated carbon emissions, water needs and wider environmental impacts are, however, mostly neglected and could lock the country into an unsustainable development path.

Bias in the attribution of forest carbon sinks pp854 - 856
Karl-Heinz Erb, Thomas Kastner, Sebastiaan Luyssaert, Richard A. Houghton, Tobias Kuemmerle, Pontus Olofsson and Helmut Haberl
doi:10.1038/nclimate2004
A substantial fraction of the terrestrial carbon sink, past and present, may be incorrectly attributed to environmental change rather than changes in forest management.

News Feature

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Providing aid before climate disasters strike pp857 - 858
Lisa Palmer
doi:10.1038/nclimate2016
Human lives can be saved when climate disaster prevention is part of international development aid.

Market Watch

Top

Pipe dream pp859 - 860
Anna Petherick
doi:10.1038/nclimate2011
Ecuador's president has called time on the Yasuní–ITT Initiative. Anna Petherick asks what the world can learn from it.

Research Highlights

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Ecological Impacts: Biological invaders | Carbon feedbacks: Oscillating in synchrony | Sea-level rise: Sinking sea | Environmental Economics: Living roofs | Decision-making: Participatory planning

News and Views

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Mitigation policy: Health co-benefits pp863 - 864
George D. Thurston
doi:10.1038/nclimate2013
Efforts to tackle climate change have met significant financial and political barriers that have been difficult to overcome. Research now shows that such measures are justified on grounds other than mitigation of climate change.
See also: Letter by J. Jason West et al.

Oceanography: Deep ocean freshening pp864 - 865
Nathaniel L. Bindoff and William R. Hobbs
doi:10.1038/nclimate2014
The traditional view of the open ocean is that surface waters should change faster and that the deep waters should be relatively stable. Now research shows that the depths of the Southern Ocean are also rapidly freshening and warming, and that these changes are spreading towards the Equator.

Carbon Storage: A permafrost carbon bomb? pp865 - 867
Claire C. Treat and Steve Frolking
doi:10.1038/nclimate2010
The fate of permafrost soil carbon following thaw depends on hydrology.
See also: Letter by Bo Elberling et al.

Soil carbon: Microbes and global carbon pp867 - 868
Joshua Schimel
doi:10.1038/nclimate2015
The amount of organic material that microbes assimilate into their biomass is critical in regulating whether soils, the planet's main pool of organic matter, will absorb or emit carbon in a warmer world.
See also: Letter by William R. Wieder et al.

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Perspective

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Benefits of tree mixes in carbon plantings pp869 - 874
Kristin B. Hulvey, Richard J. Hobbs, Rachel J. Standish, David B. Lindenmayer, Lori Lach and Michael P. Perring
doi:10.1038/nclimate1862
Trees can provide a multitude of ecosystem services. The current push to plant trees, motivated by the goal of sequestering carbon, raises the question of how tree diversity affects carbon sequestration and other services offered by afforestation/reforestation projects. This Perspective examines the potential benefits of mixed tree planting over a monoculture approach.

Review

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The role of satellite remote sensing in climate change studies pp875 - 883
Jun Yang, Peng Gong, Rong Fu, Minghua Zhang, Jingming Chen, Shunlin Liang, Bing Xu, Jiancheng Shi and Robert Dickinson
doi:10.1038/nclimate1908
Satellite remote sensing has advanced the understanding of the climate system in the short period of observations. This study highlights remote sensing discoveries that were not detected by climate models or conventional observations, and suggests future challenges for the robust determination of climate trends.

Letters

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Co-benefits of mitigating global greenhouse gas emissions for future air quality and human health pp885 - 889
J. Jason West, Steven J. Smith, Raquel A. Silva, Vaishali Naik, Yuqiang Zhang, Zachariah Adelman, Meridith M. Fry, Susan Anenberg, Larry W. Horowitz and Jean-Francois Lamarque
doi:10.1038/nclimate2009
Mitigation of greenhouse gas emissions often reduces co-emitted air pollutants, with advantages for human health. Avoided mortality from air pollution, a co-benefit of CO2 abatement, is estimated under global climate change mitigation scenarios to be in the range of US$50–US$380 per tonne of CO2. This exceeds the projected mitigation costs for 2030 and 2050, and is within the lower range of costs expected in 2100.
See also: News and Views by George D. Thurston

Long-term CO2 production following permafrost thaw pp890 - 894
Bo Elberling, Anders Michelsen, Christina Schädel, Edward A. G. Schuur, Hanne H. Christiansen, Louise Berg, Mikkel P. Tamstorf and Charlotte Sigsgaard
doi:10.1038/nclimate1955
The long-term loss of carbon from thawing permafrost in Northeast Greenland is quantified for 1996–2008 by repeated sediment sampling and incubation. Although the active layer has increased by >1 cm per year, there has not been a detectable decline in carbon stocks. Laboratory studies highlight the potential for fast carbon mobilization under aerobic conditions, but indicate that carbon at near-saturated conditions may remain largely immobilized for decades.
See also: News and Views by Claire C. Treat and Steve Frolking

Observed changes in the albedo of the Arctic sea-ice zone for the period 1982–2009 pp895 - 898
Aku Riihelä, Terhikki Manninen and Vesa Laine
doi:10.1038/nclimate1963
Albedo is a key component in the energy budget of the Arctic region, and a thorough understanding of it is essential for climate modelling. An analysis of the changes in Arctic sea-ice from 1982 to 2009 indicates that late summer sea-ice albedo is becoming dimmer. The rate of albedo decrease is shown to be accelerating over the study period.

Adapted conservation measures are required to save the Iberian lynx in a changing climate pp899 - 903
D. A. Fordham, H. R. Akçakaya, B. W. Brook, A. Rodríguez, P. C. Alves, E. Civantos, M. Triviño, M. J. Watts and M. B. Araújo
doi:10.1038/nclimate1954
The Iberian lynx has suffered severe population declines in the twentieth century. An ecological modelling study that accounts for the effects of climate change, prey availability and management intervention now shows that lynx are likely to become extinct in the wild in the next 50 years. However, a carefully planned reintroduction program could avert extinction this century.

Prediction of seasonal climate-induced variations in global food production pp904 - 908
Toshichika Iizumi, Hirofumi Sakuma, Masayuki Yokozawa, Jing-Jia Luo, Andrew J. Challinor, Molly E. Brown, Gen Sakurai and Toshio Yamagata
doi:10.1038/nclimate1945
Increasing volatility in food markets and the rising incidence of climatic extremes could lead to more frequent spikes in food prices. A global assessment of the reliability of crop simulations in reproducing past failures in major crop types suggests that seasonal forecasts can be useful for monitoring global food production.

Global soil carbon projections are improved by modelling microbial processes pp909 - 912
William R. Wieder, Gordon B. Bonan and Steven D. Allison
doi:10.1038/nclimate1951
Earth system models (ESMs) generally have crude representations of the responses of soil carbon responses to changing climate. Now an ESM that explicitly represents microbial soil carbon cycling mechanisms is able to simulate carbon pools that closely match observations. Projections from this model produce a much wider range of soil carbon responses to climate change over the twenty-first century than conventional ESMs.
See also: News and Views by Joshua Schimel

Coastal habitats shield people and property from sea-level rise and storms pp913 - 918
Katie K. Arkema, Greg Guannel, Gregory Verutes, Spencer A. Wood, Anne Guerry, Mary Ruckelshaus, Peter Kareiva, Martin Lacayo and Jessica M. Silver
doi:10.1038/nclimate1944
Extreme weather, rising seas and degraded coastal ecosystems all play a part in escalating the risks that coastal regions are exposed to. Now research into hazards facing the contiguous USA indicates that the likelihood and magnitude of losses can be reduced by intact reefs and coastal vegetation.

Global imprint of climate change on marine life pp919 - 925
Elvira S. Poloczanska, Christopher J. Brown, William J. Sydeman, Wolfgang Kiessling, David S. Schoeman, Pippa J. Moore, Keith Brander, John F. Bruno, Lauren B. Buckley, Michael T. Burrows, Carlos M. Duarte, Benjamin S. Halpern, Johnna Holding, Carrie V. Kappel, Mary I. O’Connor, John M. Pandolfi, Camille Parmesan, Franklin Schwing, Sarah Ann Thompson and Anthony J. Richardson
doi:10.1038/nclimate1958
Research that combines all available studies of biological responses to regional and global climate change shows that 81–83% of all observations were consistent with the expected impacts of climate change. These findings were replicated across taxa and oceanic basins.

Articles

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Attributing the increase in atmospheric CO2 to emitters and absorbers pp926 - 930
P. Ciais, T. Gasser, J. D. Paris, K. Caldeira, M. R. Raupach, J. G. Canadell, A. Patwardhan, P. Friedlingstein, S. L. Piao and V. Gitz
doi:10.1038/nclimate1942
There is no single correct procedure for the attribution of responsibility for growth in atmospheric CO2 concentrations because results are closely dependant on how carbon sinks are accounted for and linked to emissions. Now research that uses two different approaches—one assuming geographically constrained sinks and the other unconstrained—unambiguously attributes the largest share of the historical increase in CO2 to developed countries.

Future distribution of tundra refugia in northern Alaska pp931 - 938
Andrew G. Hope, Eric Waltari, David C. Payer, Joseph A. Cook and Sandra L. Talbot
doi:10.1038/nclimate1926
Communities of boreal species are spreading northwards as tundra communities recede under climate change in the Arctic. Concurrently, human activities in the Arctic are increasing. This study takes a multidisclinary approach to investigate the potential future distribution of tundra species and to relate the location of refugial areas to disparate land-use practices in northern Alaska.

 
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