TABLE OF CONTENTS |
January 2013 Volume 6, Issue 1 |
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| Editorial Correspondence In the press Features Books and Arts Research Highlights News and Views Correction Letters Articles Corrigendum
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Editorial | Top |
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Five years on p1 doi:10.1038/ngeo1704 With this issue, we are celebrating the fifth anniversary of the launch of Nature Geoscience — a good time to look at some numbers.
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Correspondence | Top |
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Overestimated water storage p3 Leonard F. Konikow doi:10.1038/ngeo1659 See also: Letter by Pokhrel et al. |
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Reply to 'Overestimated water storage' pp3 - 4 Yadu N. Pokhrel, Naota Hanasaki, Pat J.-F. Yeh, Tomohito J. Yamada, Shinjiro Kanae & Taikan Oki doi:10.1038/ngeo1688
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Water vapour affects both rain and aerosol optical depth pp4 - 5 Olivier Boucher and Johannes Quaas doi:10.1038/ngeo1692
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Reply to 'Water vapour affects both rain and aerosol optical depth' p5 Ilan Koren, Orit Altaratz, Lorraine A. Remer, Graham Feingold, J. Vanderlei Martins & Reuven Heiblum doi:10.1038/ngeo1693
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In the press | Top |
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Washington shake-up p6 Nicola Jones doi:10.1038/ngeo1689
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Features | Top |
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Five years of Earth science p7 doi:10.1038/ngeo1697
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Adapting the assessments pp7 - 8 Thomas F. Stocker doi:10.1038/ngeo1678 The current assessment of climate change is nearing completion. It is now time to consider how best to provide increasingly complex climate information to policymakers, suggests Thomas F. Stocker.
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The epoch of humans pp8 - 9 Jan Zalasiewicz doi:10.1038/ngeo1674 People have changed the world irrevocably. Jan Zalasiewicz discusses whether formalization of the Anthropocene as an epoch in geological time will help us understand our place in Earth history.
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The mystery of atmospheric oxygen pp9 - 10 James Kasting doi:10.1038/ngeo1684 Readily available O2 is vital to life as we know it. James Kasting looks at how and when the first whiffs of oxygen began to reach the Earth's atmosphere.
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The great sea-ice dwindle pp10 - 11 Marika Holland doi:10.1038/ngeo1681 Record minima in Arctic summer sea ice have been trumping each other. Marika Holland reflects on the likely fate of the northern sea ice cap.
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Megathrust surprises pp11 - 12 Kelin Wang doi:10.1038/ngeo1682 Numerous earthquakes have occurred at subduction zones in the past 5 years, and some were devastating. Kelin Wang describes what we have learned about the seismicity of the shallow zone.
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A steep learning curve pp12 - 13 Ulf Riebesell doi:10.1038/ngeo1690 Ocean acidification, caused by the uptake of anthropogenic carbon dioxide, is a significant stressor to marine life. Ulf Riebesell charts the rapid rise in ocean acidification research, from the discovery of its adverse effects to its entry into the political consciousness.
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Freshwater in flux pp13 - 14 Jonathan Cole doi:10.1038/ngeo1696 A surprising fraction of Earth's element cycling takes place in inland waters. Jonathan Cole suggests that interactions between these water bodies and the terrestrial biosphere are more extensive and interesting than previously thought.
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A crowded Solar System pp14 - 15 Barbara Cohen doi:10.1038/ngeo1694 The last five years have seen a boom in exploration of the Solar System. Barbara Cohen explains that the biggest gains have been right here on Earth.
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A sensitivity to history pp15 - 16 Matthew Huber doi:10.1038/ngeo1695 Questions about the sensitivity of Earth's climate to greenhouse gas forcing challenge our understanding of climate change. Matthew Huber looks at what we can learn from past greenhouse periods.
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Books and Arts | Top |
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Water and life p17 Frédéric Frappart reviews Water: All That Matters by Paul Younger doi:10.1038/ngeo1672
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Research Highlights | Top |
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Planetary science: Landscapes on Titan | Deep earth: Core light elements | Biogeochemistry: Toxic sediments | Tectonics: Accretionary surge |
News and Views | Top |
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Correction | Top |
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Hydroelectric carbon sequestration p5 doi:10.1038/ngeo1705 See also: Correspondence by Mendonca et al. |
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Letters | Top |
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Variations of sulphur dioxide at the cloud top of Venus's dynamic atmosphere pp25 - 28 Emmanuel Marcq, Jean-Loup Bertaux, Franck Montmessin & Denis Belyaev doi:10.1038/ngeo1650 A pulse of sulphur dioxide in Venus's upper atmosphere was observed by the Pioneer Venus spacecraft in the 1970s and 1980s and attributed to volcanism. Recent sulphur dioxide measurements from Venus Express indicate decadal-scale fluctuations in sulphur dioxide above Venus's cloud tops in an atmosphere that is more dynamic than expected. See also: News and Views by Esposito |
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Reduction of electron density in the night-time lower ionosphere in response to a thunderstorm pp29 - 33 Xuan-Min Shao, Erin H. Lay & Abram R. Jacobson doi:10.1038/ngeo1668 Tropospheric thunderstorms have been reported to disturb the lower ionosphere, at altitudes of 65–90 km. The use of lightning signals from a distant mesoscale storm to probe the lower ionosphere above a small tropospheric thunderstorm reveals a reduction in ionospheric electron density in response to lightning discharges in the small storm.
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The impact of polar mesoscale storms on northeast Atlantic Ocean circulation pp34 - 37 Alan Condron & Ian A. Renfrew doi:10.1038/ngeo1661 Every year, thousands of mesoscale storms (termed polar lows) cross the climatically sensitive subpolar North Atlantic Ocean. High-resolution numerical simulations of the ocean circulation, taking into account the effect of these storms on deep-water formation, suggest that polar lows significantly affect the global ocean circulation.
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Increased water storage in North America and Scandinavia from GRACE gravity data pp38 - 42 Hansheng Wang, Lulu Jia, Holger Steffen, Patrick Wu, Liming Jiang, Houtse Hsu, Longwei Xiang, Zhiyong Wang & Bo Hu doi:10.1038/ngeo1652 Changes in continental water storage have been difficult to constrain from space-borne gravity data in regions experiencing both ice melting and glacial isostatic adjustment. Separation of the hydrologic and isostatic signals reveals increases in water storage in both North America and Scandinavia over the past decade.
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Multiple causes of interannual sea surface temperature variability in the equatorial Atlantic Ocean pp43 - 47 Ingo Richter, Swadhin K. Behera, Yukio Masumoto, Bunmei Taguchi, Hideharu Sasaki & Toshio Yamagata doi:10.1038/ngeo1660 The tropical Atlantic Ocean shows sea surface temperature variability on interannual timescales. Observational and model data suggest that some of this variability can be attributed to the advection of anomalously warm northern subtropical waters toward the Equator. See also: News and Views by Lübbecke |
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Routes to energy dissipation for geostrophic flows in the Southern Ocean pp48 - 51 Maxim Nikurashin, Geoffrey K. Vallis & Alistair Adcroft doi:10.1038/ngeo1657 Wind power inputs at the surface ocean are dissipated through smaller-scale processes in the ocean interior and turbulent boundary layer. Simulations suggest that seafloor topography enhances turbulent mixing and energy dissipation in the ocean interior.
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Two pulses of extinction during the Permian-Triassic crisis pp52 - 56 Haijun Song, Paul B. Wignall, Jinnan Tong & Hongfu Yin doi:10.1038/ngeo1649 Over 90% of marine species were lost during the end-Permian extinction. Fossil data show that the crisis in China was marked by two distinct phases of marine extinction separated by a 180,000-year recovery period.
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Climatic and biotic upheavals following the end-Permian mass extinction pp57 - 60 Carlo Romano, Nicolas Goudemand, Torsten W. Vennemann, David Ware, Elke Schneebeli-Hermann, Peter A. Hochuli, Thomas Bruhwiler, Winand Brinkmann & Hugo Bucher doi:10.1038/ngeo1667 The recovery from the end-Permian mass extinction was slow and prolonged. A temperature reconstruction shows that further biotic crises during the recovery were associated with extreme warmth.
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Neoarchaean seawater sulphate concentrations from sulphur isotopes in massive sulphide ore pp61 - 64 J. W. Jamieson, B. A. Wing, J. Farquhar & M. D. Hannington doi:10.1038/ngeo1647 Sulphate concentrations in the ocean prior to 2.4 Gyr ago were lower than today. The sulphur isotope systematics of 2.7-Gyr-old sulphide deposits suggests that these low concentrations were maintained by a balance between hydrothermal sources and microbial sulphate reduction.
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Articles | Top |
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Summertime climate response to mountain pine beetle disturbance in British Columbia pp65 - 70 H. Maness, P. J. Kushner & I. Fung doi:10.1038/ngeo1642 The current mountain pine beetle infestation in forests in British Columbia ranks among the largest ecological disturbances recorded to date. An analysis of remote sensing data suggests that the resultant forest loss has led to a 1 °C rise in summertime surface temperatures. See also: News and Views by Bonan |
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Primary surface ruptures of the great Himalayan earthquakes in 1934 and 1255 pp71 - 76 S. N. Sapkota, L. Bollinger, Y. Klinger, P. Tapponnier, Y. Gaudemer & D. Tiwari doi:10.1038/ngeo1669 The recurrence times of great Himalayan earthquakes are difficult to assess because they rarely rupture the surface. Field mapping and 14C dating of offset fluvial deposits are used to identify two great Himalayan quakes that ruptured the surface along the main plate boundary fault in ad 1255 and 1934. See also: News and Views by Rockwell |
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Corrigendum | Top |
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Limited latitudinal mantle plume motion for the Louisville hotspot p76 Anthony A. P. Koppers, Toshitsugu Yamazaki, Jörg Geldmacher, Jeffrey S. Gee, Nicola Pressling, Hiroyuki Hoshi, L. Anderson, C. Beier, D. M. Buchs, L-H. Chen, B. E. Cohen, F. Deschamps, M. J. Dorais, D. Ebuna, S. Ehmann, J. G. Fitton, P. M. Fulton, E. Ganbat, C. Hamelin, T. Hanyu, L. Kalnins, J. Kell, S. Machida, J. J. Mahoney, K. Moriya, A. R. L. Nichols, S. Rausch, S-i. Sano, J. B. Sylvan & R. Williams doi:10.1038/ngeo1677 See also: Article by Koppers et al. |
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