TABLE OF CONTENTS |
May 2015 Volume 8, Issue 5 |
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| Editorial Books and Arts News and Views Perspectives Letters Articles
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Editorial | Top |
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Planetary rite of spring p329 doi:10.1038/ngeo2441 Research on the Solar System's planets has moved beyond fly-by science. Long-term observations of planetary bodies can yield insights as the days, seasons and years pass.
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Books and Arts | Top |
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Wind-swept planets p330 Nicholas Lancaster reviews Dune Worlds: How Windblown Sand Shapes Planetary Landscapes by Ralph D. Lorenz and James R. Zimbelman doi:10.1038/ngeo2428
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News and Views | Top |
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| | | Geoscience JOBS of the week | | | | | | | |
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Perspectives | Top |
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Strong influence of westerly wind bursts on El Niño diversity pp339 - 345 Dake Chen, Tao Lian, Congbin Fu, Mark A. Cane, Youmin Tang et al. doi:10.1038/ngeo2399 El Niño diversity and its genesis are debated. An overview of existing work along with a fuzzy clustering analysis and simulations suggest that the asymmetry, irregularity and extremes of El Niño result from westerly wind bursts.
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Missing iris effect as a possible cause of muted hydrological change and high climate sensitivity in models pp346 - 351 Thorsten Mauritsen and Bjorn Stevens doi:10.1038/ngeo2414 An iris effect in tropical cloud-cover was controversially proposed as a negative climate change feedback that is not represented in climate models. If such an effect exists, it could go some way to reconciling climate models and observations.
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Letters | Top |
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Darkening of Mercury's surface by cometary carbon pp352 - 356 Megan Bruck Syal, Peter H. Schultz and Miriam A. Riner doi:10.1038/ngeo2397 Mercury's surface is darker than expected given its low iron content. The delivery of cometary carbon to Mercury in micrometeorite impacts may explain the planet's globally low reflectance.
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Transient liquid water and water activity at Gale crater on Mars pp357 - 361 F. Javier Martin-Torres, Maria-Paz Zorzano, Patricia Valentin-Serrano, Ari-Matti Harri, Maria Genzer et al. doi:10.1038/ngeo2412 Liquid water on equatorial Mars is inconsistent with large-scale climatic conditions. Humidity and temperature measurements by the Curiosity rover support the formation of subsurface liquid brines by hydration of perchlorates during the night.
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Methane storms as a driver of Titan's dune orientation pp362 - 366 Benjamin Charnay, Erika Barth, Scot Rafkin, Clement Narteau, Sebastien Lebonnois et al. doi:10.1038/ngeo2406 Titan's equatorial dunes propagate eastwards, whereas Titan's surface winds blow towards the West. Atmospheric simulations suggest that tropical methane storms generate strong eastward gusts that may dominate sand transport on Titan's surface. See also: News and Views by Newman |
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Tree mortality predicted from drought-induced vascular damage pp367 - 371 William R. L. Anderegg, Alan Flint, Cho-ying Huang, Lorraine Flint, Joseph A. Berry et al. doi:10.1038/ngeo2400 Forests may be vulnerable to future droughts. A tree mortality threshold based on plant hydraulics suggests that increased drought may trigger widespread dieback in the southwestern United States by mid-century.
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Projected deglaciation of western Canada in the twenty-first century pp372 - 377 Garry K. C. Clarke, Alexander H. Jarosch, Faron S. Anslow, Valentina Radić and Brian Menounos doi:10.1038/ngeo2407 The glaciers in western Canada are experiencing rapid mass loss. Projections of their fate with a model that couples physics-based ice dynamics with a surface mass balance model suggest that glacier volume will shrink by 70% by 2100. See also: News and Views by Vieli |
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Water column methanotrophy controlled by a rapid oceanographic switch pp378 - 382 Lea Steinle, Carolyn A. Graves, Tina Treude, Bénédicte Ferré, Arne Biastoch et al. doi:10.1038/ngeo2420 Methanotrophic bacteria can consume methane emitted from the ocean floor before it reaches the atmosphere. Variations in coastal currents can reduce methane oxidation in the ocean by limiting methanotroph residence time above methane seeps.
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Links between atmospheric carbon dioxide, the land carbon reservoir and climate over the past millennium pp383 - 387 Thomas K. Bauska, Fortunat Joos, Alan C. Mix, Raphael Roth, Jinho Ahn et al. doi:10.1038/ngeo2422 Atmospheric CO2 concentrations varied on multidecadal timescales over the past millennium. Measurements of the carbon isotope composition of ice core CO2 suggest climate-driven changes in land carbon stores caused these fluctuations. See also: News and Views by Kaplan |
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Dual continental rift systems generated by plume–lithosphere interaction pp388 - 392 A. Koptev, E. Calais, E. Burov, S. Leroy and T. Gerya doi:10.1038/ngeo2401 Continental breakup can occur with or without extensive magmatic activity. Numerical simulations show that magmatic and amagmatic rifts can develop in the same tectonic setting, if a rising mantle plume is deflected to one side of the continent.
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Deformation–related volcanism in the Pacific Ocean linked to the Hawaiian–Emperor bend pp393 - 397 John M. O'Connor, Kaj Hoernle, R. Dietmar Muller, Jason P. Morgan, Nathaniel P. Butterworth et al. doi:10.1038/ngeo2416 The Hawaiian–Emperor volcanic chain has a distinctive bend. Geochemical analyses show that lavas erupted on the ocean floor close to the bend formed during deformation of the Pacific Plate, implying the bend was caused by changes in plate motion.
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Articles | Top |
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Moist convection in hydrogen atmospheres and the frequency of Saturn's giant storms pp398 - 403 Cheng Li and Andrew P. Ingersoll doi:10.1038/ngeo2405 Over the past 140 years, planet-encircling storms have occurred on Saturn about every 30 years. A sufficiently wet troposphere can explain the suppression of moist convection and storm recurrence interval on Saturn.
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Slab melting beneath the Cascade Arc driven by dehydration of altered oceanic peridotite pp404 - 408 K. J. Walowski, P. J. Wallace, E. H. Hauri, I. Wada and M. A. Clynne doi:10.1038/ngeo2417 Fluid transport in subduction zones is complex. Geochemical analysis of lavas from the Cascade Arc shows that dehydration of the deep slab interior can trigger melting in the outer part of the subducting slab in young, hot subduction zones.
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Low friction and fault weakening revealed by rising sensitivity of tremor to tidal stress pp409 - 415 Heidi Houston doi:10.1038/ngeo2419 At subduction zones, deep parts of the fault can slip slowly, generating tremor. Analysis of tremor in Cascadia reveals increasing sensitivity of slip to tidal stresses over several days, implying that the fault is weak, and weakens as it slips. See also: News and Views by Bürgmann |
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