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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 | |
Editorial | |
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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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Feature | |
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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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