Search results for "niv"

showing 10 items of 7213 documents

Incised valleys and tidal seaways: the example of the Miocene Uzès-Castillon basin, SE France.

2012

Abstract The sedimentology and stratigraphy of the Miocene deposits of the Uzès-Castillon basin are revisited. This basin, located in SE France at the junction between the perialpine foreland basin and the W Mediterranean margin, sits in a syncline that formed during the latest Cretaceous Pyrenean tectonic phase. It records the succession of shallow-water mixed siliciclastic to dominantly bioclastic carbonates that alternate with shelf marls. The clastic carbonates were accumulated as a stack of subtidal dunes and bars that were formed by tidal currents channelized in a seaway following the syncline axis. The marls indicate deposition in more protected and locally deeper waters, as interflu…

010504 meteorology & atmospheric sciencesIncised ValleyGeologyMioceneStructural basin010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesCretaceousTidalSedimentary depositional environmentPaleontologyShelf[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyMarlClastic carbonatesSiliciclastic14. Life underwaterSynclineFranceSedimentologyForeland basinGeology0105 earth and related environmental sciencesSeaway
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Microbiology and atmospheric processes: biological, physical and chemical characterization of aerosol particles

2008

Abstract. The interest in bioaerosols has traditionally been linked to health hazards for humans, animals and plants. However, several components of bioaerosols exhibit physical properties of great significance for cloud processes, such as ice nucleation and cloud condensation. To gain a better understanding of their influence on climate, it is therefore important to determine the composition, concentration, seasonal fluctuation, regional diversity and evolution of bioaerosols. In this paper, we will review briefly the existing techniques for detection, quantification, physical and chemical analysis of biological particles, attempting to bridge physical, chemical and biological methods for …

010504 meteorology & atmospheric sciencesIndoor bioaerosollcsh:LifeBiological particles[SDU.STU]Sciences of the Universe [physics]/Earth SciencesNanotechnology[SDU.ASTR] Sciences of the Universe [physics]/Astrophysics [astro-ph]01 natural sciences[PHYS.ASTR.CO]Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO]03 medical and health scienceslcsh:QH540-549.5[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processes[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere0303 health sciences[SDU.ASTR]Sciences of the Universe [physics]/Astrophysics [astro-ph][SDU.OCEAN] Sciences of the Universe [physics]/Ocean Atmosphere030306 microbiologyChemistrylcsh:QE1-996.5[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces environmentAerosolCharacterization (materials science)lcsh:Geologylcsh:QH501-531[PHYS.ASTR.CO] Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO]13. Climate action[SDU.STU] Sciences of the Universe [physics]/Earth SciencesIce nucleuslcsh:EcologyBiochemical engineeringAerosol sampling
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ERA5-Land: A state-of-the-art global reanalysis dataset for land applications

2021

Framed within the Copernicus Climate Change Service (C3S) of the European Commission, the European Centre for Medium-Range Weather Forecasts (ECMWF) is producing an enhanced global dataset for the land component of the fifth generation of European ReAnalysis (ERA5), hereafter referred to as ERA5-Land. Once completed, the period covered will span from 1950 to the present, with continuous updates to support land monitoring applications. ERA5-Land describes the evolution of the water and energy cycles over land in a consistent manner over the production period, which, among others, could be used to analyse trends and anomalies. This is achieved through global high-resolution numerical integrat…

010504 meteorology & atmospheric sciencesLEAF-AREA0207 environmental engineering[SDU.STU]Sciences of the Universe [physics]/Earth SciencesClimate change02 engineering and technologyForcing (mathematics)SOIL-MOISTURESURFACE-TEMPERATURE01 natural sciencesLAKE PARAMETERIZATIONGE1-350Water cycle020701 environmental engineeringWEST-AFRICASATELLITENUMERICAL WEATHER PREDICTION0105 earth and related environmental sciencesQE1-996.5IN-SITUElevationGeologyOPERATIONAL IMPLEMENTATION15. Life on landNumerical weather predictionEnvironmental sciences[SDU]Sciences of the Universe [physics]13. Climate actionEarth and Environmental SciencesClimatologyTemporal resolutionSNOW MODELSGeneral Earth and Planetary SciencesEnvironmental scienceSatelliteClimate model
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Pre- and syn-eruptive geochemistry of volcanic gases from Soufriere Hills of Montserrat, West Indies

1998

International audience; Soufriere Hills fumaroles contained magmaderived volatiles before and during the eruption initiated in 1995 but also preserved a typical and quite steady hydrothermal coinposition. Chemical changes due to increased boiling and a greater input of oxidizing magmatic gas occurred only at Galway's Soufriere, the most active fumarolic field. Hydrothermal buffering of the fumaroles has been favoured by their remote location (!-2 km) froin the eruptive vents and by a preferential degassing of the uprising magma through intrusive conduits under the crater. High temperature (720øC) gas collected froin the extruding lava dome in Feb. 1996 was chemically and isotopically repres…

010504 meteorology & atmospheric sciencesLava75252 Paris cedex 05GeochemistryLSCEitaly (e-mail: pare!io010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationBritish Geological SurveyVolcanic Gaseslsce.saclay.cea.ff) PalermoCEA-CNRSImpact craterevent[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment0105 earth and related environmental sciencesevent.disaster_type[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereLGSCFrance (semetg?)ipgp.j ussieu.t¾). -SS.R. YoungLava domeIPGPFumaroleGeophysics4 place JussieuDomoMagmambox.unipa.it). 4M.p. SemetGeneral Earth and Planetary Sciences91190 GiftYvette2p. Ailard and P. Jean-BaptisteFrance (e-mail: ailardGeology
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Understanding volcanoes in the Vanuatu arc

2016

We report the first helium isotope survey of volcanic gases, hot springs and some olivine phenocrysts along the Vanuatu island arc, from Tanna in the south to Vanua Lava in the north. Low CO2 content and low He-3/He-4 ratios in thermal fluids of Epi (4.0 +/- 0.1 R-a), Efate (4.5 +/- 0.1 R-a) and Pentecost (5.3 +/- 0.5 R-a) islands coherently indicate reduced mantle gas leakage and crustal contamination by radiogenic helium on these extinct volcanic systems of the former (Pliocene) arc. Instead, presently active Vanuatu volcanoes display He-3/He-4 and C/He-3 ratios typical of subduction-related volcanic arcs: He-3/He-4 ratios range from 6.4 +/- 0.5 Ra in southernmost Tanna and 7.23 +/- 0.09 …

010504 meteorology & atmospheric sciencesLavaEarth scienceGeochemistryVanuatu arcHelium isotopes[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysics01 natural sciencesVolcanic fluidsVolcanic GasesGeochemistry and Petrologyevent0105 earth and related environmental sciencesBasaltevent.disaster_typegeographygeography.geographical_feature_categoryVolcanic arcHotspot contributionFumaroleExtinct and active volcanoesMantle sourceSettore GEO/08 - Geochimica E VulcanologiaGeophysicsVolcano13. Climate actionVanuatu arc Volcanic fluids Helium isotopes Extinct and active volcanoes Mantle source Hotspot contributionIsland arcPhenocrystGeology
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Antisana volcano: A representative andesitic volcano of the eastern cordillera of Ecuador: Petrography, chemistry, tephra and glacial stratigraphy

2017

Antisana volcano is representative of many active andesitic strato-volcanoes of Pleistocene age in Ecuador's Eastern Cordillera. This study represents the first modern geological and volcanological investigation of Antisana since the late 1890's; it also summarizes the present geochemical understanding of its genesis. The volcano's development includes the formation and destruction of two older edifices (Antisana I and II) during some 400 + ka. Antisana II suffered a sector collapse about 15,000 years ago which was followed by the birth and growth of Antisana III. During its short life Antisana III has generated >= 50 eruptions of small to medium intensity, often associated with andesitic t…

010504 meteorology & atmospheric sciencesLavaEarth scienceGeochemistryengineering.material010502 geochemistry & geophysics01 natural sciencesLong-lived evolving andesitic volcanism[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyPlagioclaseTephra0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categorybiologyAndesitesAndesiteNorthern Volcanic ZoneGeologybiology.organism_classificationVolcano13. Climate actionAntisanaMagmaengineeringPhenocrystGeologyJournal of South American Earth Sciences
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Sustaining persistent lava lakes: Observations from high-resolution gas measurements at Villarrica volcano, Chile

2016

International audience; Active lava lakes – as the exposed upper part of magmatic columns – are prime locations to investigate the conduit flow processes operating at active, degassing volcanoes. Persistent lava lakes require a constant influx of heat to sustain a molten state at the Earth's surface. Several mechanisms have been proposed to explain how such heat transfer can operate efficiently. These models make contrasting predictions with respect to the flow dynamics in volcanic conduits and should result in dissimilar volatile emissions at the surface. Here we look at high-frequency SO2 fluxes, plume composition, thermal emissions and aerial video footage from the Villarrica lava lake i…

010504 meteorology & atmospheric sciencesLavaEarth scienceUAVUV camera010502 geochemistry & geophysics01 natural sciencesElectrical conduitFlux (metallurgy)Geochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyPetrologyGeophysic0105 earth and related environmental sciencesgeographyTrail By Firegeography.geographical_feature_categoryTrail ByLava domeFireconduit dynamicPlumeGeophysicsVolcano13. Climate actionSpace and Planetary ScienceGas slugMagmavolcanic degassingGeologyMulti-GAS
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Prodigious emission rates and magma degassing budget of major, trace and radioactive volatile species from Ambrym basaltic volcano, Vanuatu island Arc

2016

Abstract Ambrym volcano, in the Vanuatu arc, is one of the most active volcanoes of the Southwest Pacific region, where persistent lava lake and/or Strombolian activity sustains voluminous gas plume emissions. Here we report on the first comprehensive budget for the discharge of major, minor, trace and radioactive volatile species from Ambrym volcano, as well as the first data for volatiles dissolved in its basaltic magma (olivine-hosted melt inclusions). In situ MultiGAS analysis of H 2 O, CO 2 , SO 2 and H 2 S in crater rim emissions, coupled with filter-pack determination of SO 2 , halogens, stable and radioactive metals demonstrates a common magmatic source for volcanic gases emitted by…

010504 meteorology & atmospheric sciencesLavaGeochemistryMineralogy[SDU.STU]Sciences of the Universe [physics]/Earth SciencesAmbrymVolatile fluxes010502 geochemistry & geophysics01 natural sciencesVolcanic GasesMagma reservoirVanuatuVolatile fluxeGeochemistry and PetrologyCalderaeventGeophysicComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesMelt inclusionsBasaltevent.disaster_typegeographygeography.geographical_feature_categoryMagma degassing budgetStrombolian eruptionGeophysicsVolcano13. Climate actionIsland arcRadioactive disequilibriaGeology
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Thematic vent opening probability maps and hazard assessment of small-scale pyroclastic density currents in the San Salvador volcanic complex (El Sal…

2021

The San Salvador volcanic complex (El Salvador) and Nejapa-Chiltepe volcanic complex (Nicaragua) have been characterized by a significant variability in eruption style and vent location. Densely inhabited cities are built on them and their surroundings, including the metropolitan areas of San Salvador (∼2.4 million people) and Managua (∼1.4 million people), respectively. In this study we present novel vent opening probability maps for these volcanic complexes, which are based on a multi-model approach that relies on kernel density estimators. In particular, we present thematic vent opening maps, i.e., we consider different hazardous phenomena separately, including lava emission, small-scale…

010504 meteorology & atmospheric sciencesLavaPyroclastic rockVolcanismHazard analysis010502 geochemistry & geophysicsHazard mapvolcanic hazard mapping01 natural sciencesEnvironmental technology. Sanitary engineeringGPhreatomagmatic eruptionGeography. Anthropology. Recreation[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyGE1-350TD1-10660105 earth and related environmental sciencesgeographyQE1-996.5geography.geographical_feature_categoryGeologyEnvironmental sciencesThematic mapVolcano13. Climate actionGeneral Earth and Planetary Sciencesvent opening hazard map San Salvador volcano Nejapa-Chiltepe volcanic zoneGeologySeismology
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Shallow vent architecture during hybrid explosive-effusive activity at Cordón Caulle (Chile, 2011-12): Evidence from direct observations and pyroclas…

2013

International audience; In June 2011, an eruption of rhyolite magma began at the Puyehue-Cordón Caulle volcanic complex, southern Chile. By January 2012, explosive activity had declined from sustained pyroclastic (Plinian to sub-Plinian) fountaining to mixed gas and ash jetting punctuated by Vulcanian blasts. This explosive activity was accompanied by synchronous effusion of obsidian lava in a hybrid explosive-effusive eruption. Fortuitous climatic conditions permitted ground-based observation and video recording of transient vent dynamics as well as real-time collection of proximal juvenile ash as it sedimented from the active plume. The main eruptive vent complex and site of lava effusion…

010504 meteorology & atmospheric sciencesLava[SDE.MCG]Environmental Sciences/Global ChangesSilicicPyroclastic rockMineralogyrhyolite010502 geochemistry & geophysics01 natural sciencestube pumiceobsidianGeochemistry and PetrologyPuyehue-Cordón CaulleRhyolite[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyTephraPetrology0105 earth and related environmental sciencesgeographyVulcanian eruptiongeography.geographical_feature_categoryPeléan eruptionexplosive-effusive transitionGeophysicsVolcanopermeabilityGeologyVulcanian
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