Friday, December 21, 2012

Nature Climate Change Contents January 2013 Volume 3 Number 1 pp 1-87

Nature Chemistry
TABLE OF CONTENTS

January 2013 Volume 3, Issue 1

Editorial
Correspondence
Commentary
News Feature
Interview
Policy Watch
Research Highlights
News and Views
Perspectives
Review
Letters
Article

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Editorial

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In need of action p1
doi:10.1038/nclimate1802
Policymakers struggle to agree on new binding climate commitments and science warns time is already short if we are to avoid dangerous global warming.

Correspondence

Top

Lifting livestock's long shadow p2
Robert Goodland
doi:10.1038/nclimate1755
See also: News Feature by Anna Petherick

Climate warming and Mediterranean seagrass pp2 - 3
Cristian R. Altaba
doi:10.1038/nclimate1757
See also: Letter by Gabriel Jordà et al.

Climate warming and Mediterranean seagrass pp3 - 4
Gabriel Jordà, Núria Marbà and Carlos M. Duarte
doi:10.1038/nclimate1766
See also: Letter by Gabriel Jordà et al.

Commentary

Top

The challenge to keep global warming below 2 °C pp4 - 6
Glen P. Peters, Robbie M. Andrew, Tom Boden, Josep G. Canadell, Philippe Ciais, Corinne Le Quéré, Gregg Marland, Michael R. Raupach and Charlie Wilson
doi:10.1038/nclimate1783
The latest carbon dioxide emissions continue to track the high end of emission scenarios, making it even less likely global warming will stay below 2 °C. A shift to a 2 °C pathway requires immediate significant and sustained global mitigation, with a probable reliance on net negative emissions in the longer term.

News Feature

Top

The muddled progressive pp7 - 9
Anna Petherick
doi:10.1038/nclimate1794
Brazil has been a voice for, and a green influence on, developing countries in the past, but will that continue?

Interview

Top

Water at a crossroads pp11 - 12
doi:10.1038/nclimate1780
Climate and water expert Pavel Kabat — director and CEO of the International Institute for Applied System Analysis in Austria — calls for a long-term system approach to water research, new partnerships with the developing world and a change in donor practices, to tackle water-climate issues. He talks to Nature Climate Change.

Policy Watch

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Round two for EU climate policy pp13 - 14
Sonja van Renssen
doi:10.1038/nclimate1792
A reformed carbon market is the only agreed priority among European policymakers for 2030, but the transport sector will need to change as well, explains Sonja van Renssen

Research Highlights

Top

Ocean acidification: Aragonite shell damage | Methane emissions: Controls on Arctic methane | Human impacts: Climate–conflict nexus | Paleoclimate: Reconstructing temperature | Atmospheric science: Stilling air

News and Views

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Atmospheric science: Wetting the Arctic pp17 - 18
Tara J. Troy
doi:10.1038/nclimate1790
Streamflow from northern Eurasia into the Arctic Ocean has been increasing since the 1930s. Research shows that increased poleward moisture transport is responsible for additional water in the region.
See also: Letter by Xiangdong Zhang et al.

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Perspectives

Top

Interpreting trade-related CO2 emission transfers pp19 - 23
Michael Jakob and Robert Marschinski
doi:10.1038/nclimate1630
Most industrialized countries import more carbon emissions, through the products they buy abroad, than they export by selling domestic products overseas, with implications for global emissions and the design of carbon trade policies. A new method unravels the determinants of these emission transfers to understand how international trade affects global emissions and the associated policy implications.

The impacts of climate change on terrestrial Earth surface systems pp24 - 29
Jasper Knight and Stephan Harrison
doi:10.1038/nclimate1660
Assessment and managment of the impacts of climate change on Earth surface systems such as glaciers, rivers and mountains are somewhat neglected in national and international climate policy initiatives. It is argued in this Perspective that this is a critical omission because Earth surface systems provide water and soil resources, sustain ecosystem services, and influence biogeochemical cycles.

Review

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Consequences of widespread tree mortality triggered by drought and temperature stress pp30 - 36
William R. L. Anderegg, Jeffrey M. Kane and Leander D. L. Anderegg
doi:10.1038/nclimate1635
The multitude of forest die-off events within the last decade strongly suggests that forest mortality is an emerging global phenomenon, constituting a major uncertainty in projections of climate impacts on terrestrial ecosystems, climate-ecosystem interactions, and carbon-cycle feedbacks. This Review considers the societal and ecological consequences of dying forests.

Letters

Top

Summer-time climate impacts of projected megapolitan expansion in Arizona pp37 - 41
M. Georgescu, M. Moustaoui, A. Mahalov and J. Dudhia
doi:10.1038/nclimate1656
Regional climates can be modified by urban development affecting the radiation and hydrological balances. This study looks at the expanding megapolitan area in the Sun Corridor, Arizona, USA, and models local climate change in line with urban development.

All flavours of El Niño have similar early subsurface origins pp42 - 46
Nandini Ramesh and Raghu Murtugudde
doi:10.1038/nclimate1600
The El Niño/Southern Oscillation (ENSO) is the dominant mode of climate variability. This study identifies a critical process that remains constant through ENSO regime shifts and that begins many months before the peak of the event. The findings should help understand how ENSO will respond to a warming world.

Enhanced poleward moisture transport and amplified northern high-latitude wetting trend pp47 - 51
Xiangdong Zhang, Juanxiong He, Jing Zhang, Igor Polyakov, Rüdiger Gerdes, Jun Inoue and Peili Wu
doi:10.1038/nclimate1631
Increasing Eurasian Arctic river discharges and climate model projections show an increased wetting trend in northern high latitudes in coming years. Now a study finds that the increase in river discharge has accelerated in the past decade and that enhancement of poleward atmospheric moisture transport decisively contributes to this increase.
See also: News and Views by Tara J. Troy

Increasing drought under global warming in observations and models pp52 - 58
Aiguo Dai
doi:10.1038/nclimate1633
Historical records show increased aridity over many land areas since 1950. This study looks at observations and model projections from 1923 to 2010, to test the ability of models to predict future drought conditions. Models are able to capture the greenhouse-gas forcing and El Niño–Southern Oscillation mode for historical periods, which inspires confidence in their projections of drought.

Anthropogenic influence on multidecadal changes in reconstructed global evapotranspiration pp59 - 62
H. Douville, A. Ribes, B. Decharme, R. Alkama and J. Sheffield
doi:10.1038/nclimate1632
Understanding the response of evapotranspiration to global warming should help to predict surface climate, including heatwaves and droughts. This study shows that increasing atmospheric concentrations of greenhouse gases and decreasing loadings of anthropogenic (and volcanic) aerosols have led to enhanced evapotranspiration in mid and high latitudes over recent decades.

Global diversity of drought tolerance and grassland climate-change resilience pp63 - 67
Joseph M. Craine, Troy W. Ocheltree, Jesse B. Nippert, E. Gene Towne, Adam M. Skibbe, Steven W. Kembel and Joseph E. Fargione
doi:10.1038/nclimate1634
Grasslands have always experienced drought, but future drought conditions are likely to be more severe and frequent as climates change. This study shows that many of the world’s grasslands probably have drought-tolerant grasses that can maintain ecosystem functions, and the resilience of grasslands globally requires the maintenance of grass diversity.

Adaptation of US maize to temperature variations pp68 - 72
Ethan E. Butler and Peter Huybers
doi:10.1038/nclimate1585
Predictions of climate warming raise concerns about food security. However, the extent to which adaptation can offset heat-related yield losses remains unclear. Now research that used spatial adaptation of US maize crops as a surrogate for future adaptation finds that the yield reduction resulting from warming of 2 °C above pre-industrial levels can be approximately halved using existing management practices.

Emerging Vibrio risk at high latitudes in response to ocean warming pp73 - 77
Craig Baker-Austin, Joaquin A. Trinanes, Nick G. H. Taylor, Rachel Hartnell, Anja Siitonen and Jaime Martinez-Urtaza
doi:10.1038/nclimate1628
There is increasing concern about the potential role of climate change in facilitating the spread of bacterial waterborne infectious diseases to new areas. Now research supports these concerns by finding an association between long-term environmental changes observed in the Baltic area and the recent emergence of Vibrio infections in the region.

An extreme climatic event alters marine ecosystem structure in a global biodiversity hotspot pp78 - 82
Thomas Wernberg, Dan A. Smale, Fernando Tuya, Mads S. Thomsen, Timothy J. Langlois, Thibaut de Bettignies, Scott Bennett and Cecile S. Rousseaux
doi:10.1038/nclimate1627
In 2011 the waters along the west coast of Australia—a global hotspot of biodiversity—experienced an unprecedented (in recorded times) warming event with warming anomalies of 2–4 °C that persisted for more than ten weeks. Now research shows that biodiversity patterns of temperate seaweeds, invertebrates and fishes were significantly different following the warming event.

Article

Top

Climate-change impact assessment for inlet-interrupted coastlines pp83 - 87
Roshanka Ranasinghe, Trang Minh Duong, Stefan Uhlenbrook, Dano Roelvink and Marcel Stive
doi:10.1038/nclimate1664
Climate-driven sea-level rise will result in coastline retreat due to landward movement of the coastal profile. However, coastlines adjacent to tidal inlets will also be influenced by changes in the rate of basin infill and variations in rainfall. A model demonstrates that typical practice, which fails to incorporate these processes, is liable to represent only 25–50% of total coastline change.

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