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  								  								  									TABLE OF CONTENTS  									
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  								  									|   									 May 2018 Volume 8, Issue 5   									 |   								
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  								  									   |   									   Editorial    									   Correspondence    									   Comment    									   Books & Arts    									   Feature    									   Research Highlights    									   News & Views    									   Letters    									   Articles    									  |   									  									  									    									  									 |   								
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  								  									|   									    Feeling the heat      p347        									 doi:10.1038/s41558-018-0169-y    									 |   								
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  								  									    									Correspondence  									 |   									  |   								
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  								  									|   									    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    									 |   								
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  								  									    									Comment  									 |   									  |   								
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  								  									|   									    Time to refine key climate policy models      pp350 - 352        									 Alexander R. Barron    									 doi:10.1038/s41558-018-0132-y    									 |   								
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  								  								  									    									Books & Arts  									 |   									  |   								
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  								  									|   									    Texas, we have a water problem      pp353 - 354        									 Douglas Brent McRoberts    									 doi:10.1038/s41558-018-0151-8    									 |   								
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  								  									|   									    The inconvenient truth of failed climate policies      pp355 - 358        									 Sonja van Renssen    									 doi:10.1038/s41558-018-0155-4    									 |   								
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  								  									    									Research Highlights  									 |   									  |   								
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  								  									    									News & Views  									 |   									  |   								
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  								  									|   									    Spatial variation in messaging effects      pp360 - 361        									 Christopher Warshaw    									 doi:10.1038/s41558-018-0143-8    									 |   								
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  								  									|   									    A few scenarios still do not fit all      pp361 - 362        									 Vanessa Schweizer    									 doi:10.1038/s41558-018-0148-3    									 |   								
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  								  									|   									    Arctic sea ice at 1.5 and 2 °C      pp362 - 363        									 James A. Screen    									 doi:10.1038/s41558-018-0137-6    									 |   								
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  								  									|   									    A hot future for European droughts      pp364 - 365        									 Adriaan J. Teuling    									 doi:10.1038/s41558-018-0154-5    									 |   								
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  								  									|   									    Africa and the Paris Agreement      pp365 - 366        									 Andries C. Kruger    									 doi:10.1038/s41558-018-0146-5    									 |   								
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  								  									|   									    Deforestation intensifies hot days      pp366 - 368        									 Paul C. Stoy    									 doi:10.1038/s41558-018-0153-6    									 |   								
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  								  									|   									    Running dry      p369        									 Graham Simpkins    									 doi:10.1038/s41558-018-0164-3    									 |   								
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  								  									    									Letters  									 |   									  |   								
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  								  									|   									    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.   									     									    									 |   								
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  								  									|   									    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.   									     									    									 |   								
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  								  									|   									    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.   									     									    									 |   								
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  								  									|   									    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.   									     									    									 |   								
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  								  									    									Articles  									 |   									  |   								
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  								  									|   									    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.   									     									    									 |   								
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  								  									|   									    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.   									     									    									 |   								
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  								  									|   									    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.   									     									    									 |   								
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  								  									|   									    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.   									     									    									 |   								
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  								  									|   									    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.   									     									    									 |   								
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  								  									|   									    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.   									     									    									 |   								
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  								  									|   									    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.   									     									    									 |   								
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  								  									|   									    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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