Wednesday, October 29, 2014

Nature Climate Change Contents November 2014 Volume 4 Number 11 pp 931-1036

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Nature Chemistry

TABLE OF CONTENTS

November 2014 Volume 4, Issue 11

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

Top

The precious drop p931
doi:10.1038/nclimate2426
Water is a vital resource and as the climate changes so does the hydrological cycle. What this means for water availability (or excess) on the local and regional scale is key for decision makers and communities.

Correspondence

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CO2 emissions from crop residue-derived biofuels p932
Niclas Scott Bentsen, Søren Larsen and Claus Felby
doi:10.1038/nclimate2401

CO2 emissions from crop residue-derived biofuels pp932 - 933
John J. Sheehan, Paul R. Adler, Stephen J. Del Grosso, Mark Easter, William Parton, Keith Paustian and Stephen Williams
doi:10.1038/nclimate2403

CO2 emissions from crop residue-derived biofuels pp933 - 934
G. Philip Robertson, Peter R. Grace, R. César Izaurralde, William P. Parton and Xuesong Zhang
doi:10.1038/nclimate2402

Reply to 'CO2 emissions from crop residue-derived biofuels' pp934 - 935
Adam J. Liska, Haishun Yang, Matthew P. Pelton and Andrew E. Suyker
doi:10.1038/nclimate2423

Lessons learned from geoengineering freshwater systems pp935 - 936
Bryan M. Spears and Stephen C. Maberly
doi:10.1038/nclimate2412

Commentaries

Top

Getting there from here pp936 - 937
Keely B. Maxwell
doi:10.1038/nclimate2413
Institutions need to adapt to ensure coequal social and biophysical global change science.

Characterizing loss and damage from climate change pp938 - 939
Rachel James, Friederike Otto, Hannah Parker, Emily Boyd, Rosalind Cornforth, Daniel Mitchell and Myles Allen
doi:10.1038/nclimate2411
Policymakers are creating mechanisms to help developing countries cope with loss and damage from climate change, but the negotiations are largely neglecting scientific questions about what the impacts of climate change actually are.

China–Russia gas deal for a cleaner China pp940 - 942
Wenjie Dong, Wenping Yuan, Shuguang Liu, John Moore, Peijun Shi, Shengbo Feng, Jieming Chou, Xuefeng Cui and Kejun Jiang
doi:10.1038/nclimate2382
The China–Russia gas deal will play an important role in reducing greenhouse-gas emissions and air pollution in China.

China's hydrofluorocarbon challenge pp943 - 945
Junjie Zhang and Can Wang
doi:10.1038/nclimate2377
China should take more active participation in a prospective agreement on the global phase-down of hydrofluorocarbons.

The global groundwater crisis pp945 - 948
J. S. Famiglietti
doi:10.1038/nclimate2425
Groundwater depletion the world over poses a far greater threat to global water security than is currently acknowledged.

Feature

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The next water cycle pp949 - 950
Lisa Palmer
doi:10.1038/nclimate2420
Adaptation of water resources management will help communities adjust to changes in the water cycle expected with climate change, but it can't be fixed by innovations alone.

Policy Watch

Top

A bioeconomy to fight climate change pp951 - 953
Sonja van Renssen
doi:10.1038/nclimate2419
The use of biomass for energy generation is helping European Union countries meet their renewable energy and emissions targets, but demand from other sectors means policy needs to be developed for maximum climate benefits, reports Sonja van Renssen.

Correction

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Addendum: Market Watch: Cash flow p953
Anna Petherick
doi:10.1038/nclimate2416

Research Highlights

Top

Biogeochemistry: Carbon turnover | Marine biodiversity: Shifting distributions | Arctic sea ice: Eroding the coast | Adaptation: A new policy field

News and Views

Top

Physical and political impacts: Complex river boundaries at risk pp955 - 956
Shlomi Dinar
doi:10.1038/nclimate2421
Many international river basins are suffering from climate-driven impacts, with implications for national security. Now, research highlights the need to analyse shifting river boundaries to better understand potential socio-political threats.

Oceanography: Where's the heat? pp956 - 957
Gregory C. Johnson and John M. Lyman
doi:10.1038/nclimate2409
In recent decades, over nine-tenths of Earth's top-of-the-atmosphere energy imbalance has been stored in the ocean, which is rising as it warms. Combining satellite sea-level data with ocean mass data or model results allows insights into ocean warming.

Time of emergence: Moving up early detection pp958 - 959
Jianjun Yin
doi:10.1038/nclimate2422
Natural climate variability complicates the detection of anthropogenic climate change in the twenty-first century. Now, research shows that evidence of human influence first emerges from sea level rather than temperature rise.
See also: Letter by Kewei Lyu et al.

Warming trends: A flatter Earth pp959 - 960
Alexander R. Stine
doi:10.1038/nclimate2424
The regular beat of the seasons and between day and night are far more noticeable than recent increases in surface temperature. Researchers now show that these rhythms are changing in a way that parallels the pattern of long-term surface warming.
See also: Letter by George Wang & Michael E. Dillon

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Perspective

Top

Feasible mitigation actions in developing countries pp961 - 968
Michael Jakob, Jan Christoph Steckel, Stephan Klasen, Jann Lay, Nicole Grunewald, Inmaculada Martínez-Zarzoso, Sebastian Renner and Ottmar Edenhofer
doi:10.1038/nclimate2370
Energy use is crucial for economic development, but drives greenhouse-gas emissions. A low-carbon growth path requires a radical transformation of the energy system that would be too costly for developing nations. Efforts should focus on feasible mitigation actions such as fossil fuel subsidy reform, decentralized access to modern energy and fuel switching in the power sector.

Review

Top

Benthic coral reef calcium carbonate dissolution in an acidifying ocean pp969 - 976
Bradley D. Eyre, Andreas J. Andersson and Tyler Cyronak
doi:10.1038/nclimate2380
The authors of this Review argue that changes to carbonate dissolution in an acidifying ocean, which have been relatively overlooked, are potentially more important than calcification for the future accretion and survival of coral reef ecosystems.

Letters

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Effectiveness of US state policies in reducing CO2 emissions from power plants pp977 - 982
Don Grant, Kelly Bergstrand and Katrina Running
doi:10.1038/nclimate2385
In the United States, a key goal of states’ climate change policies is to reduce CO2 emissions from electric power plants. This study shows that specific policy packages significantly shape CO2 emissions from individual power plants.

Linearity between temperature peak and bioenergy CO2 emission rates pp983 - 987
Francesco Cherubini, Thomas Gasser, Ryan M. Bright, Philippe Ciais and Anders H. Strømman
doi:10.1038/nclimate2399
The characteristics of the global mean temperature response to bioenergy production systems is explored under different assumptions and emissions scenarios in the context of the 2 °C target.

Recent geographic convergence in diurnal and annual temperature cycling flattens global thermal profiles pp988 - 992
George Wang and Michael E. Dillon
doi:10.1038/nclimate2378
An analysis of a high-resolution global temperature data set shows that temperate and polar regions are becoming more tropical in their temperature variation profiles, potentially affecting organisms and impacting human agriculture and health.
See also: News and Views by Alexander R. Stine

Modelled glacier response to centennial temperature and precipitation trends on the Antarctic Peninsula pp993 - 998
Bethan J. Davies, Nicholas R. Golledge, Neil F. Glasser, Jonathan L. Carrivick, Stefan R. M. Ligtenberg, Nicholas E. Barrand, Michiel R. van den Broeke, Michael J. Hambrey and John L. Smellie
doi:10.1038/nclimate2369
The glaciers of the Antarctic Peninsula are experiencing faster melt because of increased temperatures; however, changes in precipitation may offset some of the future melt. This study looks at the relationship between glaciers and climate and finds a representative glacier is more sensitive to temperature change, rather than precipitation change. This indicates that precipitation increases are unlikely to counter the increased melt from warming.

Quantifying underestimates of long-term upper-ocean warming pp999 - 1005
Paul J. Durack, Peter J. Gleckler, Felix W. Landerer and Karl E. Taylor
doi:10.1038/nclimate2389
The ocean stores over 90% of the heat due to anthropogenic warming. This study uses satellite observations and climate models to investigate the warming of the upper ocean (0–700 m) and finds that warming is biased low, most likely because of poor Southern Hemisphere sampling. Applying adjustments results in a large increase in upper-ocean heat content estimates.

Time of emergence for regional sea-level change pp1006 - 1010
Kewei Lyu, Xuebin Zhang, John A. Church, Aimée B. A. Slangen and Jianyu Hu
doi:10.1038/nclimate2397
This work investigates when the anthropogenic signal in regional sea-level rise will emerge from natural variability. Considering thermal expansion and changes in density and circulation, 50% of the global ocean will show an anthropogenic signal by the early-to-mid 2040s, whereas when all variables are considered, the anthropogenic signal will emerge in over 50% of the global ocean by 2020. This is substantially earlier than for surface air temperature and has little dependence on emissions scenarios.
See also: News and Views by Jianjun Yin

Detection and impacts of leakage from sub-seafloor deep geological carbon dioxide storage pp1011 - 1016
Jerry Blackford, Henrik Stahl, Jonathan M. Bull, Benoît J. P. Bergès, Melis Cevatoglu, Anna Lichtschlag, Douglas Connelly, Rachael H. James, Jun Kita, Dave Long, Mark Naylor, Kiminori Shitashima, Dave Smith, Peter Taylor, Ian Wright, Maxine Akhurst, Baixin Chen, Tom M. Gernon, Chris Hauton, Masatoshi Hayashi, Hideshi Kaieda, Timothy G. Leighton, Toru Sato, Martin D. J. Sayer, Masahiro Suzumura, Karen Tait, Mark E. Vardy, Paul R. White and Steve Widdicombe
doi:10.1038/nclimate2381
This study shows that the biological impact and footprint of a leakage from a controlled sub-seabed release of carbon dioxide is confined to a few tens of metres, and identifies monitoring strategies for full-scale carbon storage operations.

Articles

Top

Determinants of stagnating carbon intensity in China pp1017 - 1023
Dabo Guan, Stephan Klasen, Klaus Hubacek, Kuishuang Feng, Zhu Liu, Kebin He, Yong Geng and Qiang Zhang
doi:10.1038/nclimate2388
A systematic analysis shows that China’s climate policy on carbon intensity reduction may not help all Chinese regions to become more efficient and could actually lock the whole nation into a long-term emission-intensive economic structure.

Adaptation of a globally important coccolithophore to ocean warming and acidification pp1024 - 1030
Lothar Schlüter, Kai T. Lohbeck, Magdalena A. Gutowska, Joachim P. Gröger, Ulf Riebesell and Thorsten B. H. Reusch
doi:10.1038/nclimate2379
Climate change is increasing ocean temperatures and acidification. This study tests the adaptive evolution of a globally important phytoplankton, Emiliania huxleyi, and finds they are able to evolve to cope with the changing marine environment.

Deep-ocean contribution to sea level and energy budget not detectable over the past decade pp1031 - 1035
W. Llovel, J. K. Willis, F. W. Landerer and I. Fukumori
doi:10.1038/nclimate2387
The global ocean is a major heat reservoir of the climate system. This study investigates ocean warming for 2005–2013 in the context of global sea-level rise and Earth’s energy budget, and finds that the deep ocean (below 2,000 m) has contributed negligibly to both.

 

Erratum

Top

Erratum: A compromise to break the climate impasse p1035
Marco Grasso and J Timmons Roberts
doi:10.1038/nclimate2417

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