Search results for "QE"

showing 10 items of 457 documents

Characterisation of the magmatic signature in gas emissions from Turrialba Volcano, Costa Rica

2014

The equilibrium composition of volcanic gases with their magma is often overprinted by interaction with a shallow hydrothermal system. Identifying the magmatic signature of volcanic gases is critical to relate their composition to properties of the magma (temperature, fO2, gas-melt segregation depth). We report measurements of the chemical composition and flux of the major gas species emitted from Turrialba Volcano during March 2013. Measurements were made of two vents in the summit region, one of which opened in 2010 and the other in 2012. We determined an average SO2 flux of 5.2 ± 1.9 kg s-1 using scanning ultraviolet spectroscopy, and molar proportions of H2O, CO2, SO2, HCl, CO and H2 ga…

010504 meteorology & atmospheric sciencesStratigraphyChemical compositionContinuous emissionSoil ScienceMineralogyVolcanoe010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationVolcanic GasesHydrothermal systemFlux (metallurgy)lcsh:StratigraphyMagmatic signaturesGeochemistry and PetrologyUltraviolet spectroscopyeventGas compositionFourier transform infrared spectroscopyChemical compositionlcsh:QE640-6990105 earth and related environmental sciencesEarth-Surface Processesevent.disaster_typegeographygeography.geographical_feature_categorylcsh:QE1-996.5Fourier transform infrared spectrometryPaleontologyFourier transform infrared spectroscopyGeologyChemical signatureGas-sensing systemlcsh:GeologyGeophysicsVolcanoCarbon dioxideSulfur dioxide13. Climate actionEquilibrium compositionMagmaCarbon dioxide; Fourier transform infrared spectroscopy; Sulfur dioxide; Ultraviolet spectroscopy; Volcanoes; Chemical compositions; Chemical signatures; Continuous emission; Equilibrium compositions; Fourier transform infrared spectrometry; Gas-sensing systems; Hydrothermal system; Magmatic signaturesGeology
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A critical discussion of the electromagnetic radiation (EMR) method to determine stress orientations within the crust

2012

Abstract. In recent years, the electromagnetic radiation (EMR) method has been used to detect faults and to determine main horizontal stress directions from variations in intensities and directional properties of electromagnetic emissions, which are assumed to be generated during micro-cracking. Based on a large data set taken from an area of about 250 000 km2 in Northern Germany, Denmark, and southern Sweden with repeated measurements at one location during a time span of about 1.5 yr, the method was systematically tested. Reproducible observations of temporary changes in the signal patterns, as well as a strongly concentric spatial pattern of the main directions of the magnetic component …

010504 meteorology & atmospheric sciencesStratigraphySoil Science010502 geochemistry & geophysicsSignalElectromagnetic radiation01 natural sciencesStress (mechanics)03 medical and health scienceslcsh:StratigraphyGeochemistry and PetrologyPoint (geometry)Very low frequencyEarth-Surface Processeslcsh:QE640-699030304 developmental biology0105 earth and related environmental sciences0303 health scienceslcsh:QE1-996.5Geovetenskap och miljövetenskapPaleontologyCrustGeologyData setlcsh:GeologyGeophysicsCommon spatial patternGeologiEarth and Related Environmental SciencesSeismologyGeology
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Implementation of a comprehensive ice crystal formation parameterization for cirrus and mixed-phase clouds in the EMAC model (based on MESSy 2.53)

2018

A comprehensive ice nucleation parameterization has been implemented in the global chemistry-climate model EMAC to improve the representation of ice crystal number concentrations (ICNCs). The parameterization of Barahona and Nenes (2009, hereafter BN09) allows for the treatment of ice nucleation taking into account the competition for water vapour between homogeneous and heterogeneous nucleation in cirrus clouds. Furthermore, the influence of chemically heterogeneous, polydisperse aerosols is considered by applying one of the multiple ice nucleating particle parameterizations which are included in BN09 to compute the heterogeneously formed ice crystals. BN09 has been modified in order to co…

010504 meteorology & atmospheric sciencesglobal climate modelNucleationMineral dustnucleation parameterizations010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesempirical parameterizationTroposphereinsoluble particlesddc:5500105 earth and related environmental sciencesmineral dustIce crystalssubmodel system messylcsh:QE1-996.5Northern Hemisphereatmospheric aerosollcsh:Geology13. Climate actionupper troposphereIce nucleusEnvironmental scienceCirrustransport sectorsWater vapordroplet number concentration
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Aseismic strain episodes at Campi Flegrei Caldera, Italy

2021

Since 2004 a research project has been developed to monitor subsurface deformation of Italian volcanoes using borehole strainmeters and long-baseline tiltmeters. Six Sacks-Evertson dilatometers were installed around Campi Flegrei caldera and Vesuvius during 2004–2005 (Scarpa et al., 2007), and in 2008 these instruments were supplemented by two arrays of 28–280 m long water-tube tiltmeters in underground tunnels. Relevant strainmeter and tiltmeter data have been collected and analysed from the instruments installed near Campi Flegrei caldera during the recent unrest episodes. In the period 2004–2005 strain, tilt and GPS data from Campi Flegrei indicate the onset of surface deformation that a…

010504 meteorology & atmospheric scienceslcsh:Dynamic and structural geologyBoreholeTiltmeterStrainmeter010502 geochemistry & geophysics01 natural sciencesCampi Flegrei ground deformationground deformationlcsh:QE500-639.5CalderaVertical displacementlcsh:Science0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryMicroseismlcsh:QE1-996.5General Medicinelcsh:GeologyVolcanoMagmalcsh:QCampi FlegreiSeismologyGeology
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A sea surface temperature reconstruction for the southern Indian Ocean trade wind belt from corals in Rodrigues Island (19°S, 63°E)

2016

Abstract. The western Indian Ocean has been warming rapidly over recent decades, causing a greater number of extreme climatic events. It is therefore of paramount importance to improve our understanding of links between Indian Ocean sea surface temperature (SST) variability, climate change and sustainability of tropical coral reef ecosystems. Here we present monthly resolved coral Sr ∕ Ca records from two different locations from Rodrigues Island (63° E, 19° S) in the south-central Indian Ocean trade wind belt. We reconstruct SST based on a linear relationship with the Sr ∕ Ca proxy with records starting from 1781 and 1945, respectively. We assess relationships between the observed long-ter…

010506 paleontology010504 meteorology & atmospheric sciences550Corallcsh:LifeClimate changeMonsoon010502 geochemistry & geophysics01 natural sciencesddc:570lcsh:QH540-549.514. Life underwaterEcology Evolution Behavior and SystematicsEarth-Surface Processes0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorySubtropical Indian Ocean Dipolelcsh:QE1-996.5Coral reeflcsh:GeologySea surface temperaturelcsh:QH501-531Oceanography13. Climate actionClimatologyIndian Ocean Dipolelcsh:EcologyGeologyTeleconnection
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Carbon accumulation rate in a raised bog in Latvia, NE Europe, in relation to climate warming

2018

The carbon accumulation rate (CAR) over the last 180 years was estimated by measuring carbon concentrations in 1-cm layers in a fine-resolution dated and analysed peat sequence in Teiči Bog, Latvia, NE Europe. We used the Granger causality test to examine the temporal (lagged) relationships between the CAR and the historical climate variables. Our results showed that the average CAR was 192 g C m–2 yr–1 during the last 180 years and 169 g C m–2 yr–1 when excluding the acrotelm where decomposition and the stock of carbon are still not in the balance. The Granger causality test showed significant positive temporal associations between the temperature and the CAR, indicating that the temperatu…

010506 paleontology010504 meteorology & atmospheric scienceslcsh:QE1-996.5Global warmingGranger causality test.chemistry.chemical_elementC/N ratio01 natural scienceslcsh:GeologySphagnumchemistryGeneral Earth and Planetary SciencesEnvironmental sciencecarbon accumulation ratepeatlandPhysical geographyCarbonRaised bog0105 earth and related environmental sciencesWater Science and TechnologyEstonian Journal of Earth Sciences
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The SISAL database: a global resource to document oxygen and carbon isotope records from speleothems

2018

Stable isotope records from speleothems provide information on past climate changes, most particularly information that can be used to reconstruct past changes in precipitation and atmospheric circulation. These records are increasingly being used to provide “out-of-sample” evaluations of isotope-enabled climate models. SISAL (Speleothem Isotope Synthesis and Analysis) is an international working group of the Past Global Changes (PAGES) project. The working group aims to provide a comprehensive compilation of speleothem isotope records for climate reconstruction and model evaluation. The SISAL database contains data for individual speleothems, grouped by cave system. Stable isotopes of oxyg…

010506 paleontologyClimate Research010504 meteorology & atmospheric sciencesClimate changeSpeleothemF800010502 geochemistry & geophysicscomputer.software_genre01 natural sciencesKlimatforskningCavePaleoclimatologylcsh:Environmental sciences0105 earth and related environmental scienceslcsh:GE1-350geographygeography.geographical_feature_categoryDatabaseStable isotope ratiospeleothemsPALEOCLIMATOLOGIAlcsh:QE1-996.5lcsh:GeologyMetadata13. Climate actionGeneral Earth and Planetary SciencesEnvironmental scienceClimate modelcomputerChronologyEarth System Science Data
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Terrestrial plants and marine algae from the Late Jurassic lithographic limestone of the Causse Méjean (Lozère, southern France)

2016

International audience; A new Late Jurassic flora was discovered in the fossiliferous lithographic limestone of the Causse Méjean, Lozère (southern France). It consists of the first Kimmeridgian/Tithonian plants from this area. Fossil plants are represented by megaremains preserved as impressions. This flora shows a co-occurrence of terrestrial plants and marine algae. The land plants include vegetative remains ascribed to bennettitaleans (Zamites Brongniart, 1828), conifers (Brachyphyllum Brongniart, 1828), and pteridosperms (Cycadopteris Zigno, 1853). Marine algae were ascribed to dasyclads (Goniolina D’Orbigny, 1850). Lithological and palaeontological features suggest preservation in a f…

010506 paleontologyFloraved/biology.organism_classification_rank.speciesLate JurassicContext (language use)010502 geochemistry & geophysics01 natural sciencesBennettitaleansBrachyphyllumPaleontologyAlgaeTerrestrial plant14. Life underwaterPteridospermsDasycladales0105 earth and related environmental sciencesZamites[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontologybiologyved/biologyEcologyDasycladslcsh:QE1-996.5PtéridospermesGeologyVegetation15. Life on landbiology.organism_classificationConifèreslcsh:GeologyConifersHabitatJurassique terminalBennettitalesBassin des Causses.[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyCausses basin.GeologyCausses basin
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Fossiliferous Holocene tufa of Mende (Lozère, southern France): implication for the Atlantic vegetation of the Causses Basin

2016

International audience; Tufas bearing plant macroremains are uncommon in the Causses Basin (southern France). Here, we report anew fossiliferous tufa deposits at Mende, in Lozère. This palaeontological site is the first Quaternary tufa from thenorthern part of the Causses Basin that yields such an abundance of plant macroremains. The radiocarbon dating showsthat these Holocene deposits are related to the Atlantic period. Geomorphology and mineralogy show that theplant-bearing deposit is a calcareous tufa only composed by calcite, deposited near to an outlet of cool water, linked tothe karstic hydrological system of the Causse de Mende. The flora exposed in this article is dominated by angio…

010506 paleontologyLeavesAngiosperms010504 meteorology & atmospheric sciencesTilia cordataStructural basin01 natural sciencesTufslaw.inventionFeuillesPaleontologyLozèrelawRadiocarbon datingCausses BasinHolocene0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontologygeographygeography.geographical_feature_categoryBassin des CaussesHolocenebiologylcsh:QE1-996.5GeologyVegetationTufasbiology.organism_classificationKarstlcsh:GeologyTufaAngiospermesQuaternary[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologyHolocène
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The Borschovo section of the Gauja and Amata regional stages (Leningrad Region, Russia): sedimentology and biostratigraphy

2018

The results of the detailed sedimentological study and bed-by-bed collecting of fossils from the Borschovo section exposing the upper Givetian–lower Frasnian boundary beds are discussed. The succession consists of sandstones alternating with argillaceous and clayey packages that contain vertebrate and plant remains in the upper part. The grain size, sedimentary structures and cross-bed orientation considerably differ in the Oredezh Beds and the Staritsa Beds. Fine- to coarse-grained cross-stratified sandstones of the Oredezh Beds most probably are fluvial deposits, whereas the sandstones of the Staritsa Beds yielding tidal structures that show variable directions of the cross-bedding were a…

010506 paleontologyMiddle–Upper Devonianbiologylcsh:QE1-996.5Biostratigraphy010502 geochemistry & geophysicsbiology.organism_classification01 natural scienceslcsh:GeologyPaleontologyAmataSection (archaeology)sedimentary environmentGeneral Earth and Planetary Sciencessiliciclastic depositsSedimentologyvertebrate assemblage.Geology0105 earth and related environmental sciencesWater Science and TechnologyEstonian Journal of Earth Sciences
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