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Open for submissions Soft sensors and actuators Guest editor: Il-Kwon Oh, KAIST, South Korea This Collection will provide a platform for interdisciplinary studies of soft sensors and actuators, including their application in smart textiles, haptic electronics, biomedical devices and soft robotics.
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TABLE OF CONTENTS
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November 2018 Volume 11, Issue 11 |
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| Editorial News & Views Review Articles Perspectives Articles Amendments & Corrections | |
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Publishing online monthly, Nature Astronomy aims to bring together astronomers, astrophysicists and planetary scientists. In addition to the latest advances in research, we offer Comment and Opinion pieces on topical subjects of relevance to our community, including the societal impact of astronomy and updates on telescopes and space missions.
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Editorial | |
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Treasures from the deep p801 doi:10.1038/s41561-018-0260-z |
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News & Views | |
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| | | Geoscience JOBS of the week | | | | | | | | | |
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Review Articles | |
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Role of air-mass transformations in exchange between the Arctic and mid-latitudes pp805 - 812 Felix Pithan, Gunilla Svensson, Rodrigo Caballero, Dmitry Chechin, Timothy W. Cronin et al. doi:10.1038/s41561-018-0234-1 Understanding the thermodynamics of air-mass transformations that occur in the atmosphere at the boundary between the Arctic and mid-latitudes is key to improving weather and climate predictions, according to a literature synthesis |
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Perspectives | |
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CO2 evasion along streams driven by groundwater inputs and geomorphic controls pp813 - 818 Clément Duvert, David E. Butman, Anne Marx, Olivier Ribolzi & Lindsay B. Hutley doi:10.1038/s41561-018-0245-y Groundwater-derived CO2 inputs and emissions along streams are highly variable in both space and time, according to measurements of dissolved CO2 from two headwater catchments. |
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True polar wander of Ceres due to heterogeneous crustal density pp819 - 824 P. Tricarico doi:10.1038/s41561-018-0232-3 The dwarf planet Ceres may have reoriented in the past due to a heterogeneously dense crust, a scenario consistent with gravity and topographic data and the distribution of crustal fractures. |
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High riverine CO2 emissions at the permafrost boundary of Western Siberia pp825 - 829 S. Serikova, O. S. Pokrovsky, P. Ala-Aho, V. Kazantsev, S. N. Kirpotin et al. doi:10.1038/s41561-018-0218-1 Rivers in the Western Siberian Lowland, the world's largest peatland, play a significant role in the release of terrestrial carbon to the atmosphere, according to in situ measurements of carbon dioxide emissions from rivers. |
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Path-dependent reductions in CO2 emission budgets caused by permafrost carbon release pp830 - 835 T. Gasser, M. Kechiar, P. Ciais, E. J. Burke, T. Kleinen et al. doi:10.1038/s41561-018-0227-0 Carbon release from permafrost thaw would substantially decrease the amount of carbon emissions required to meet climate targets, according to climate simulations. |
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Recent Southern Ocean warming and freshening driven by greenhouse gas emissions and ozone depletion pp836 - 841 Neil C. Swart, Sarah T. Gille, John C. Fyfe & Nathan P. Gillett doi:10.1038/s41561-018-0226-1 Recent warming and freshening of the Southern Ocean can be attributed to human-induced greenhouse gas emissions, with stratospheric ozone depletion also playing a role, according to a synthesis of observations and climate model simulations. |
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Large-scale impacts of the mesoscale environment on mixing from wind-driven internal waves pp842 - 847 C. B. Whalen, J. A. MacKinnon & L. D. Talley doi:10.1038/s41561-018-0213-6 Mesoscale ocean features can alter the magnitude of turbulent mixing caused by wind-driven internal waves, an analysis of Argo float and model data suggests. |
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Ice-sheet modulation of deglacial North American monsoon intensification pp848 - 852 Tripti Bhattacharya, Jessica E. Tierney, Jason A. Addison & James W. Murray doi:10.1038/s41561-018-0220-7 The intensity of the North American summer monsoon was modified by changes in the extent of the Laurentide Ice Sheet during the Last Glacial Maximum and subsequent deglaciation, according to isotope records and numerical simulations. |
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Concomitant variability in high-latitude aerosols, water isotopes and the hydrologic cycle pp853 - 859 Bradley R. Markle, Eric J. Steig, Gerard H. Roe, Gisela Winckler & Joseph R. McConnell doi:10.1038/s41561-018-0210-9 On timescales of centuries and longer, aerosol concentrations in Antarctic ice are controlled by changes in the nature of mid- and high-latitude precipitation, according to analyses of palaeoclimate data. |
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A highly resolved record of relative sea level in the western Mediterranean Sea during the last interglacial period pp860 - 864 Victor J. Polyak, Bogdan P. Onac, Joan J. Fornós, Carling Hay, Yemane Asmerom et al. doi:10.1038/s41561-018-0222-5 A sea-level record from Mallorca shows no evidence of large, millennial-scale oscillations during the last interglacial. |
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Crustal inheritance and a top-down control on arc magmatism at Mount St Helens pp865 - 870 Paul A. Bedrosian, Jared R. Peacock, Esteban Bowles-Martinez, Adam Schultz & Graham J. Hill doi:10.1038/s41561-018-0217-2 Crustal structures are as important as deep mantle melting in controlling magma ascent and the composition and distribution of erupted material, according to 3D resistivity modelling, geophysical data and the distribution of Quaternary volcanism. |
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Locking on a megathrust as a cause of distributed faulting and fault-jumping earthquakes pp871 - 875 Simon Lamb, Richard Arnold & James D. P. Moore doi:10.1038/s41561-018-0230-5 Earthquakes that jump from fault to fault in subduction zones can be explained by locking on the plate interface, according to GPS data from New Zealand where the 2016 Kaikoura earthquake produced a complex array of crustal ruptures. |
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Slab stagnation due to a reduced viscosity layer beneath the mantle transition zone pp876 - 881 Wei Mao & Shijie Zhong doi:10.1038/s41561-018-0225-2 Slab stagnation in the transition zone is explained by a thin, weak layer and is transient on timescales of tens of millions of years, according to a global mantle convection model that includes phase changes and plate motion history. |
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Amendments & Corrections | |
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Author Correction: Carbon budgets for 1.5 and 2°C targets lowered by natural wetland and permafrost feedbacks pp882 - 886 Edward Comyn-Platt, Garry Hayman, Chris Huntingford, Sarah E. Chadburn, Eleanor J. Burke et al. doi:10.1038/s41561-018-0247-9 |
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