TABLE OF CONTENTS
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April 2015 Volume 8, Issue 4 |
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| Editorial Correspondence Commentaries Books and Arts News and Views Perspective Letters Articles
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Editorial | Top |
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Eruption trials p241 doi:10.1038/ngeo2415 The eruption of Mount Tambora in 1815 has been linked to climate change and social unrest. Such historical eruptions could serve as test cases for models used to assess future climate changes. |
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Correspondence | Top |
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Icelandic volcanic emissions and climate p243 Andrew Gettelman, Anja Schmidt & Jón Egill Kristjansson doi:10.1038/ngeo2376 |
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Commentaries | Top |
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Eruption politics pp244 - 245 Clive Oppenheimer doi:10.1038/ngeo2408 The impact of a volcanic eruption depends on more than just its size. We need more interdisciplinary research to understand the global societal consequences of past and future volcanic eruptions. |
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The year without a summer pp246 - 248 J. Luterbacher & C. Pfister doi:10.1038/ngeo2404 The 1815 eruption of Tambora caused an unusually cold summer in much of Europe in 1816. The extreme weather led to poor harvests and malnutrition, but also demonstrated the capability of humans to adapt and help others in worse conditions. |
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Tying down eruption risk pp248 - 250 Stephen Self & Ralf Gertisser doi:10.1038/ngeo2403 200 years after the eruption of Mount Tambora, the eruption volume remains poorly known, as is true for other volcanic eruptions over past millennia. We need better records of size and occurrence if we are to predict future large eruptions more accurately. |
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Books and Arts | Top |
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Volcanoes past and present p251 Amy Whitchurch & Alicia Newton review Volcanism and Global Environmental Change edited by Anja Schmidt, Kirsten E. Fristad and Linda T. Elkins-Tanton doi:10.1038/ngeo2409 |
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Wringing food from the world p252 Prabhu Pingali reviews The Big Ratchet: How Humanity Thrives in the Face of Natural Crisis by Ruth DeFries doi:10.1038/ngeo2410 |
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News and Views | Top |
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Perspective | Top |
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Clouds, circulation and climate sensitivity pp261 - 268 Sandrine Bony, Bjorn Stevens, Dargan M. W. Frierson, Christian Jakob, Masa Kageyama et al. doi:10.1038/ngeo2398 Our understanding of the interactions between clouds, circulation and climate is limited. Four central research questions — now tractable through advances in models, concepts and observations — are proposed to accelerate future progress. |
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Letters | Top |
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Impact vaporization of planetesimal cores in the late stages of planet formation pp269 - 272 Richard G. Kraus, Seth Root, Raymond W. Lemke, Sarah T. Stewart, Stein B. Jacobsen et al. doi:10.1038/ngeo2369 Differentiated planetesimals may have delivered iron-rich material to Earth in giant impacts at the end of accretion. Impact experiments suggest that the planetesimals' iron cores vaporized, aiding dispersal and mixing into Earth's mantle. See also: News and Views by Anderson |
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Ice nucleation by cellulose and its potential contribution to ice formation in clouds pp273 - 277 N. Hiranuma, O. Mohler, K. Yamashita, T. Tajiri, A. Saito et al. doi:10.1038/ngeo2374 Some biological particles act as ice nuclei in the atmosphere, affecting clouds and precipitation. Cloud-chamber experiments demonstrate that cellulose particles can act as efficient ice-nucleating particles in supercooled clouds. |
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Influence of the El Niño/Southern Oscillation on tornado and hail frequency in the United States pp278 - 283 John T. Allen, Michael K. Tippett & Adam H. Sobel doi:10.1038/ngeo2385 The El Niño/Southern Oscillation modulates global weather and climate. Analyses of large-scale environmental indices show that it also affects the frequency of tornado and hail events in the central United States, which may help with predictability. |
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Photosynthetic seasonality of global tropical forests constrained by hydroclimate pp284 - 289 Kaiyu Guan, Ming Pan, Haibin Li, Adam Wolf, Jin Wu et al. doi:10.1038/ngeo2382 Droughts can cause dry-season productivity to decline in tropical forests. This decline occurs when precipitation is below 2,000 mm yr-1, resulting in insufficient subsurface water storage to maintain constant production through the dry season. |
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Substantial contribution of biomethylation to aquifer arsenic cycling pp290 - 293 Scott C. Maguffin, Matthew F. Kirk, Ashley R. Daigle, Stephen R. Hinkle & Qusheng Jin doi:10.1038/ngeo2383 Arsenic in aquifers is transformed by biological and abiotic reactions. Field measurements and laboratory experiments suggest that the microbial methylation of arsenic contributes to subsurface arsenic cycling. |
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Ocean access to a cavity beneath Totten Glacier in East Antarctica pp294 - 298 J. S. Greenbaum, D. D. Blankenship, D. A. Young, T. G. Richter, J. L. Roberts et al. doi:10.1038/ngeo2388 Totten Glacier has the largest thinning rate in East Antarctica. A derivation of the sea floor bathymetry reveals entrances to the ice cavity beneath the glacier that could allow deep warm water to enter and enhance basal melting. See also: News and Views by Fretwell |
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Presence of oxygen and aerobic communities from sea floor to basement in deep-sea sediments pp299 - 304 Steven D'Hondt, Fumio Inagaki, Carlos Alvarez Zarikian, Lewis J. Abrams, Nathalie Dubois et al. doi:10.1038/ngeo2387 The depth of oxygen penetration and microbial activity in marine sediments varies by region. Sediment cores from the South Pacific Gyre host oxygen and aerobic microbial communities to at least 75 metres below the sea floor. See also: News and Views by Orcutt |
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Amplification of bedrock canyon incision by wind pp305 - 310 Jonathan P. Perkins, Noah J. Finnegan & Shanaka L. de Silva doi:10.1038/ngeo2381 Water is considered the primary agent that erodes and shapes bedrock canyons. Analyses of canyon morphology in the central Andes suggest that abrasion by wind can amplify canyon incision and reshape canyons on Earth—and possibly on Mars. See also: News and Views by Perron |
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Slab stagnation in the shallow lower mantle linked to an increase in mantle viscosity pp311 - 314 Hauke Marquardt & Lowell Miyagi doi:10.1038/ngeo2393 Subducting slabs can stagnate in the lower mantle. High-pressure laboratory experiments show that the viscosity of a dominant mantle phase increases dramatically at shallow lower-mantle depths, which could cause the slabs to halt their descent. See also: News and Views by Cordier |
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Articles | Top |
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Dynamics of the intertropical convergence zone over the western Pacific during the Little Ice Age pp315 - 320 Hong Yan, Wei Wei, Willie Soon, Zhisheng An, Weijian Zhou et al. doi:10.1038/ngeo2375 Precipitation patterns in the western Pacific changed at the onset of the Little Ice Age. A synthesis of precipitation reconstructions suggests that this change resulted from a contraction of the intertropical convergence zone. |
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Continental crust generated in oceanic arcs pp321 - 327 Esteban Gazel, Jorden L. Hayes, Kaj Hoernle, Peter Kelemen, Erik Everson et al. doi:10.1038/ngeo2392 The origin of continental crust is unclear. Geochemical and geophysical analyses of the Central American land bridge show that continental crust began to form there when enriched oceanic crust created above the Galapagos plume was subducted. |
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