Wednesday, April 29, 2015

Nature Geoscience contents: May 2015 Volume 8 Number 5 pp329-415

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Nature Geoscience

TABLE OF CONTENTS

May 2015 Volume 8, Issue 5

Editorial
Books and Arts
News and Views
Perspectives
Letters
Articles
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Editorial

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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.

Books and Arts

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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

News and Views

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Seismology: Diary of a wimpy fault   pp331 - 332
Roland Bürgmann
doi:10.1038/ngeo2426
Subduction zone faults can slip slowly, generating tremor. The varying correlation between tidal stresses and tremor occurring deep in the Cascadia subduction zone suggests that the fault is inherently weak, and gets weaker as it slips.
See also: Article by Houston

Glacier change: Dynamic projections   pp332 - 333
Andreas Vieli
doi:10.1038/ngeo2425
Mountain glaciers around the world are in decay. According to a modelling study that — unusually — includes full ice flow physics, those in Western Canada will largely be restricted to the coastal region by the year 2100.
See also: Letter by Clarke et al.

Planetary science: Stormy origins of Titan's dunes   pp334 - 335
Claire Newman
doi:10.1038/ngeo2423
Titan's equatorial dunes seem to move in the opposite direction to the prevailing easterly winds. Infrequent methane storms at Titan's low latitudes may briefly couple surface winds to fast westerlies above, dominating the net movement of sand.
See also: Letter by Charnay et al.

Holocene carbon cycle: Climate or humans?   pp335 - 336
Jed O. Kaplan
doi:10.1038/ngeo2432
Analyses of ice-core carbon isotopes show that variations in atmospheric CO2 levels during the past millennium are controlled by changes in land reservoirs. But whether climate variations or human activity were mainly responsible is uncertain.
See also: Letter by Bauska et al.

Volcanology: Electric eruption   p337
Amy Whitchurch
doi:10.1038/ngeo2435

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Perspectives

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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.

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.

Letters

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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.

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.

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

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.

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

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.

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

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.

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.

Articles

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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.

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.

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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