Monday, April 30, 2018

Nature Climate Change Contents: May 2018 Volume 8 Number 5

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TABLE OF CONTENTS

May 2018 Volume 8, Issue 5

Editorial
Correspondence
Comment
Books & Arts
Feature
Research Highlights
News & Views
Letters
Articles
 
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Editorial

 

Feeling the heat    p347
doi:10.1038/s41558-018-0169-y

Correspondence

 

Cascading biases against poorer countries    pp348 - 349
Sivan Kartha, Tom Athanasiou, Simon Caney, Elizabeth Cripps, Kate Dooley et al.
doi:10.1038/s41558-018-0152-7

Comment

 

Time to refine key climate policy models    pp350 - 352
Alexander R. Barron
doi:10.1038/s41558-018-0132-y

Books & Arts

 

Texas, we have a water problem    pp353 - 354
Douglas Brent McRoberts
doi:10.1038/s41558-018-0151-8

Feature

 

The inconvenient truth of failed climate policies    pp355 - 358
Sonja van Renssen
doi:10.1038/s41558-018-0155-4

Research Highlights

 

Come rain or shine    p359
Alastair Brown
doi:10.1038/s41558-018-0165-2

Unequal exposure    p359
Adam Yeeles
doi:10.1038/s41558-018-0166-1

Taking a closer look    p359
Bronwyn Wake
doi:10.1038/s41558-018-0167-0

Disappearing Andean snow    p359
Graham Simpkins
doi:10.1038/s41558-018-0168-z

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News & Views

 

Spatial variation in messaging effects    pp360 - 361
Christopher Warshaw
doi:10.1038/s41558-018-0143-8

A few scenarios still do not fit all    pp361 - 362
Vanessa Schweizer
doi:10.1038/s41558-018-0148-3

Arctic sea ice at 1.5 and 2 °C    pp362 - 363
James A. Screen
doi:10.1038/s41558-018-0137-6

A hot future for European droughts    pp364 - 365
Adriaan J. Teuling
doi:10.1038/s41558-018-0154-5

Africa and the Paris Agreement    pp365 - 366
Andries C. Kruger
doi:10.1038/s41558-018-0146-5

Deforestation intensifies hot days    pp366 - 368
Paul C. Stoy
doi:10.1038/s41558-018-0153-6

Running dry    p369
Graham Simpkins
doi:10.1038/s41558-018-0164-3

Letters

 

Experimental effects of climate messages vary geographically    pp370 - 374
Baobao Zhang, Sander van der Linden, Matto Mildenberger, Jennifer R. Marlon, Peter D. Howe et al.
doi:10.1038/s41558-018-0122-0

Geographic variation in social, economic, political and climatic factors may influence public responsiveness to climate change messaging. This study shows that messages about scientific consensus have a greater influence in more conservative US states.

 

Record-breaking climate extremes in Africa under stabilized 1.5°C and 2°C global warming scenarios    pp375 - 380
Shingirai Nangombe, Tianjun Zhou, Wenxia Zhang, Bo Wu, Shuai Hu et al.
doi:10.1038/s41558-018-0145-6

The record hot year of 2015 in Africa had devastating impacts. The likelihood of future annual temperature extremes over Africa exceeding those of 2015 are 91% and 100% in 1.5°C and 2°C worlds, respectively, stressing the benefits of limiting future anthropogenic warming.

 

Future equivalent of 2010 Russian heatwave intensified by weakening soil moisture constraints    pp381 - 385
L. M. Rasmijn, G. van der Schrier, R. Bintanja, J. Barkmeijer, A. Sterl et al.
doi:10.1038/s41558-018-0114-0

The 2010 Russia heatwave had devastating impacts, including loss of life, wildfire and drought. Model simulations reveal similar heatwaves may be amplified by up to 8°C in the future as soil moisture becomes less able to suppress maximum temperatures.

 

Historical deforestation locally increased the intensity of hot days in northern mid-latitudes    pp386 - 390

doi:10.1038/s41558-018-0131-z

Deforestation in the northern mid-latitudes has generally been considered to cause biogeophysical changes that drive mean annual cooling in the region. Research now suggests that historical deforestation has led to substantial local warming of hot days.

 

Articles

 

Alternative pathways to the 1.5°C target reduce the need for negative emission technologies    pp391 - 397
Detlef P. van Vuuren, Elke Stehfest, David E. H. J. Gernaat, Maarten van den Berg, David L. Bijl et al.
doi:10.1038/s41558-018-0119-8

Scenarios that constrain warming to 1.5°C currently place a large emphasis on CO2 removal. Alternative pathways involving lifestyle change, rapid electrification and reduction of non-CO2 gases could reduce the need for such negative emission technologies.

 

Air quality co-benefits of carbon pricing in China    pp398 - 403
Mingwei Li, Da Zhang, Chiao-Ting Li, Kathleen M. Mulvaney, Noelle E. Selin et al.
doi:10.1038/s41558-018-0139-4

The co-benefits of carbon pricing in China are investigated by a cross-scale modelling approach. The health benefits from reduced emissions and improved air quality could offset the climate policy costs.

 

Ice-free Arctic projections under the Paris Agreement    pp404 - 408
Michael Sigmond, John C. Fyfe & Neil C. Swart
doi:10.1038/s41558-018-0124-y

Nations are currently pursuing efforts to constrain anthropogenic warming to 1.5°C. In such a world, model projections suggest the Arctic will be ice-free every one in forty years, compared to one in every five under stabilized 2°C warming.

 

Reduced probability of ice-free summers for 1.5°C compared to 2°C warming    pp409 - 413
Alexandra Jahn
doi:10.1038/s41558-018-0127-8

Arctic sea ice cover has declined significantly in recent years. Model simulations suggest the probability of an ice-free Arctic will be 100% under 2°C, but 30% under 1.5°C, motivating efforts to constrain anthropogenic warming.

 

Early emergence of anthropogenically forced heat waves in the western United States and Great Lakes    pp414 - 420
Hosmay Lopez, Robert West, Shenfu Dong, Gustavo Goni, Ben Kirtman et al.
doi:10.1038/s41558-018-0116-y

Heat waves have become increasingly frequent in the United States, but their occurrence is largely linked to natural variability. Model simulations reveal anthropogenically forced signals will first emerge in the western United States and Great Lakes regions by ~2030.

 

Anthropogenic warming exacerbates European soil moisture droughts    pp421 - 426
L. Samaniego, S. Thober, R. Kumar, N. Wanders, O. Rakovec et al.
doi:10.1038/s41558-018-0138-5

Severe drought plagued Europe in 2003, amplifying heatwave conditions that killed more than 30,000 people. Assuming business as usual, such soil moisture deficits will become twice as frequent in the future and affect up to two-thirds of the European population.

 

Increasing precipitation volatility in twenty-first-century California    pp427 - 433
Daniel L. Swain, Baird Langenbrunner, J. David Neelin & Alex Hall
doi:10.1038/s41558-018-0140-y

California recently experienced a rapid shift from multi-year drought to abundant rainfall. A large ensemble of climate model simulations suggests that the frequency of extreme wet-to-dry precipitation events will increase by 25% to 100% across California due to anthropogenic forcing.

 

Forest response to rising CO2 drives zonally asymmetric rainfall change over tropical land    pp434 - 440
Gabriel J. Kooperman, Yang Chen, Forrest M. Hoffman, Charles D. Koven, Keith Lindsay et al.
doi:10.1038/s41558-018-0144-7

Increasing zonal asymmetry in tropical precipitation is projected by 2100, with increases over Asian and African forests and decreases over South American forests. Plant physiological responses to increasing CO2 are now identified as a primary driving mechanism.

 

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