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showing 10 items of 34508 documents

Reaction path models of magmatic gas scrubbing

2016

Gas-water-rock reactions taking place within volcano-hosted hydrothermal systems scrub reactive, water-soluble species (sulfur, halogens) from the magmatic gas phase, and as such play a major control on the composition of surface gas manifestations. A number of quantitative models of magmatic gas scrubbing have been proposed in the past, but no systematic comparison of model results with observations from natural systems has been carried out, to date. Here, we present the results of novel numerical simulations, in which we initialized models of hydrothermal gas-water-rock at conditions relevant to Icelandic volcanism. We focus on Iceland as an example of a "wet" volcanic region where scrubb…

010504 meteorology & atmospheric sciencesIcelandMineralogychemistry.chemical_elementVolcanism010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationGas phaseHydrothermal systemGeochemistry and PetrologyReaction path0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryEQ3/6GeologyGas emissionsGas-water-rock interactionSulfurMagmatic gas scrubbing; Gas-water-rock interaction; EQ3/6; Hydrothermal systems; IcelandMagmatic gas scrubbingSettore GEO/08 - Geochimica E VulcanologiachemistryVolcano13. Climate actionGeologyData scrubbing
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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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High time resolution fluctuations in volcanic carbon dioxide degassing from Mount Etna

2014

Abstract We report here on the first record of carbon dioxide gas emission rates from a volcano, captured at ≈ 1 Hz. These data were acquired with a novel technique, based on the integration of UV camera observations (to measure SO2 emission rates) and field portable gas analyser readings of plume CO2/SO2 ratios. Our measurements were performedat the North East crater of Mount Etna, southern Italy, and the data reveal strong variability in CO2 emissions over timescales of tens to hundreds of seconds, spanning two orders of magnitude. This carries importantimplications for attempts to constrain global volcanic CO2 release to the atmosphere, and will lead to an increased insight into short te…

010504 meteorology & atmospheric sciencesLagPlume imagingInduced seismicity010502 geochemistry & geophysicsAtmospheric sciencesPassive degassing01 natural sciencesAtmospherechemistry.chemical_compoundImpact craterGeochemistry and Petrology0105 earth and related environmental sciencesCarbon dioxide; Passive degassing; Plume imaging; Volcanic remote sensing; Volcano seismology; Geophysics; Geochemistry and PetrologyBasaltgeographygeography.geographical_feature_categoryVolcano seismologyPlumeVolcanic remote sensingGeophysicsVolcanochemistryCarbon dioxide13. Climate actionCarbon dioxideCarbon dioxide; Passive degassing; Plume imaging; Volcanic remote sensing; Volcano seismology; Geochemistry and Petrology; GeophysicsSeismologyGeology
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Estimating high resolution evapotranspiration from disaggregated thermal images

2016

Abstract Accurate evapotranspiration (ET) estimations based on surface energy balance from remote sensing require information in the thermal infrared (TIR) domain, normally provided with an insufficient spatial resolution. In order to estimate ET in heterogeneous agricultural areas, we inspect in this paper the use of disaggregation techniques applied to two different sensors, such as MODIS (daily revisit cycle and 1 km spatial resolution in the TIR domain) and Spot 5 (5 days revisit cycle and 10 m spatial resolution in the VNIR bands but no TIR band). Spot 5 images were used as a proxy for upcoming Sentinel-2. The Simplified Two-Source Energy Balance (STSEB) model was used for the estimati…

010504 meteorology & atmospheric sciencesLand surface temperatureMeteorology0211 other engineering and technologiesEnergy balanceSoil ScienceHigh resolutionGeology02 engineering and technologySensible heat01 natural sciencesVNIREvapotranspirationThermalEnvironmental scienceComputers in Earth SciencesImage resolution021101 geological & geomatics engineering0105 earth and related environmental sciencesRemote sensingRemote Sensing of Environment
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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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Using mosses as biomonitors to study trace element emissions and their distribution in six different volcanic areas

2017

Volcanoes emit SO2, CO2, and H2S, but also trace elements gases and particles such as As, Cd, Cr, Cu, Hg, Ni, Pb, and Sb. Active moss bag biomonitoring, an easy to apply and low budget method, was used to determine trace element release from volcanic areas of different geological context and climates. Exposure height variations (0.7–1.6 m above ground) due to different availability of natural tie points did not affect the results. Accumulation was linear for exposure durations from three days to nine weeks, so values were comparable by normalization to moss exposure time. Uncovered moss bags showed higher accumulation than co-exposed covered ones because of additional dust and wet deposit…

010504 meteorology & atmospheric sciencesLavaMineralogyContext (language use)010501 environmental sciences01 natural sciencesVolcanic GasesGeochemistry and PetrologyBiomonitoringeventGeophysicVolatiles0105 earth and related environmental sciencesevent.disaster_typeVolatile elementVolcanic emissiongeographygeography.geographical_feature_categorybiologyTrace elementActive biomonitoringbiology.organism_classificationMossGeophysicsVolcanoMetal(loid)GeologyJournal of Volcanology and Geothermal Research
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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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