Search results for "Climate Action"

showing 10 items of 2410 documents

A Pluto-like radius and a high albedo for the dwarf planet Eris from an occultation

2011

The dwarf planet Eris is a trans-Neptunian object with an orbital eccentricity of 0.44, an inclination of 44 degrees and a surface composition very similar to that of Pluto. It resides at present at 95.7 astronomical units (1ĝ€‰au is the Earth-Sun distance) from Earth, near its aphelion and more than three times farther than Pluto. Owing to this great distance, measuring its size or detecting a putative atmosphere is difficult. Here we report the observation of a multi-chord stellar occultation by Eris on 6 November 2010 ut. The event is consistent with a spherical shape for Eris, with radius 1,163±6 kilometres, density 2.52±0.05 grams per cm 3 and a high visible geometric albedo,. No nitro…

010504 meteorology & atmospheric sciences[PHYS.ASTR.EP]Physics [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP]Ciencias FísicasAstronomical unitDwarf planet[SDU.ASTR.EP]Sciences of the Universe [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP]Orbital eccentricityAstrophysicsno utilizado01 natural sciences7. Clean energyOccultationdwarf planetAtmosphere0103 physical sciencesTrans-Neptunian object010303 astronomy & astrophysicsEris0105 earth and related environmental sciencesPhysicsMultidisciplinarybiologyPlutoAstronomybiology.organism_classificationPlutoAstronomíaEris13. Climate actionCIENCIAS NATURALES Y EXACTASalbedo
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Evolution of the neodymium isotopic signature of neritic seawater on a northwestern Pacific margin: new constrains on possible end-members for the co…

2013

11 pages; International audience; The Neodymium(Nd) isotope composition of fish remains has beenwidely used to track past changes in oceanic circulation. Although the number of published Nd isotope data for the Cretaceous has markedly increased in the last years, no consensus has been reached on the structure of the oceanic circulation and its evolution during the Late Cretaceous. Yet this period is characterised bymajor geodynamical and climatic changes andmarked by the disappearance of global oceanic anoxic events inwhich changes in oceanic circulation modesmay have played a significant role. In this study we present the first record of Nd isotopic composition of fish remains from contine…

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global Changes010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesCretaceousIsotopic signaturePaleontologyContinental marginJapanGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistryoceanic circulation14. Life underwater[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography0105 earth and related environmental sciencesRadiogenic nuclide[ SDU.STU.OC ] Sciences of the Universe [physics]/Earth Sciences/OceanographyOcean currentGeology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistrySeafloor spreadingCretaceous[ SDE.MCG ] Environmental Sciences/Global Changes13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyPeriod (geology)Seawaterneodymium isotopesGeology
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13C composition of dissolved organic carbon in upland forested catchments of the Morvan Mountains (France): Influence of coniferous and deciduous veg…

2007

10 pages; International audience; One of the main environmental changes caused by human activities is that of land use. These changes influence the quantity and quality of the dissolved organic matter (DOM) fluxes through the vegetation–soil–stream system. The aim of this work is to evaluate the influence of the substitution of native deciduous forests by well managed coniferous forests on dissolved organic carbon (DOC) fluxes and their associated carbon isotopic composition (d13CDOC). DOC fluxes and d13CDOC were monitored for 2 years in the streams of four similar upland forested catchments in the Morvan Mountains (France). Mean annual DOC concentrations and fluxes were 2–4 times lower in …

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesDrainage basinSTREAMS01 natural sciences[ SDE.MCG.CPE ] Environmental Sciences/Global Changes/domain_sde.mcg.cpeStream water[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryDissolved organic carbon[ SDE.MCG.SIC ] Environmental Sciences/Global Changes/domain_sde.mcg.sic[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environment[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentChemical composition0105 earth and related environmental sciencesWater Science and TechnologyStable isotopesHydrologygeographySoil organic mattergeography.geographical_feature_category[SDE.MCG.SIC]Environmental Sciences/Global Changes/domain_sde.mcg.sicSoil organic matter04 agricultural and veterinary sciencesVegetation15. Life on land[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistry[SDE.MCG.CPE]Environmental Sciences/Global Changes/domain_sde.mcg.cpe[ SDE.MCG ] Environmental Sciences/Global ChangesDeciduous13. Climate actionSoil solutionSoil water040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceDissolved organic carbon
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The Early-Cambrian Boho volcano of the El Graara massif, Morocco: Petrology, geodynamic setting and coeval sedimentation

2006

15 pages; International audience; A major volcanic episode is recorded across the Neoproterozoic-Cambrian transition in the Moroccan Anti-Atlas. Several volcanic cones are still preserved in the El Graara massif, laterally correlatable with volcanic flows dated as Early Cambrian (U/Pb date of 534 ± 10 Ma). Volcanic ashes and flows are interbedded with the uppermost part of the Adoudou dolostones, whereas the best-preserved volcano (the Boho Jbel) is onlapped by the overlying Lie-de-vin strata. Available petro-geochemical data from the Boho volcano suggest an alkaline magmatism probably derived from low-grade melting of a garnet–lherzolite mantle source, followed by fractional crystallizatio…

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesGeochemistrySlope apron[ SDU.STU.VO ] Sciences of the Universe [physics]/Earth Sciences/Volcanology010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphySyenites01 natural sciencesDiagenesisLower CambrianBreccia[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyAlkaline basaltsPetrologySlope aponComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface Processes[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyBasaltgeographygeography.geographical_feature_categoryTerrigenous sedimentGeologyMassifDiagenesis[ SDE.MCG ] Environmental Sciences/Global ChangesMoroccoVolcano13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphySubaerial[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/Paleontology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyVolcanic coneGeology
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Occurrence of fossil organic matter in modern environments: optical, geochemical and isotopic evidence

2011

International audience; This study relates to the input and fate of fossil organic matter (FOM) in the modern environment, and focuses on two experimental watersheds overlying Jurassic marls: Le Laval and Le Brusquet (1 km(2) in area), located near Digne, Alpes-de-Haute-Provence, France. Considering that FOM delivery is mainly a result of different processes affecting sedimentary rocks [(bio)chemical and mechanical weathering], samples from different pools were collected: bedrocks, weathering profiles, soils and riverine particles. The samples were examined using complementary techniques: optical (palynofacies methods), geochemical (Rock-Eval 6 pyrolysis, C/N ratio), molecular (gas chromato…

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesMineralogyWeatheringatmospheric carbon010502 geochemistry & geophysics01 natural sciencesstorageGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryMarlEnvironmental ChemistryOrganic matterglobal carbon balance0105 earth and related environmental scienceschemistry.chemical_classificationvariabilitysedimentary-rocks[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryerosionPollutionPalynofaciesALPES DE HAUTE PROVENCE[ SDE.MCG ] Environmental Sciences/Global Changesmarine-sedimentschemistry13. Climate actionSoil waterrock-eval pyrolysis[SDE]Environmental SciencesErosionSedimentary rockmodern soilshaute-provencePyrolysisGeology
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Chlorine Partitioning Between a Basaltic Melt and H2O-CO2 Fluids at Mount Etna

2009

Partitioning experiments between a basaltic melt from Mt. Etna and a low-density hydrous fluid or vapor containing H(2)O or H(2)O-CO(2) were performed at 1200-1260 degrees C, at pressures between 1 and 200 MPa, either near the nickel-nickel oxide (NNO) buffer or at two log units above it (NNO + 2), and with different chloride concentrations. Most of the experiments were done at chloride-brine-undersaturated conditions, although at the highest Cl concentrations explored brine saturation might have been reached. The average partition coefficients (D(Cl)(fluid/melt)) over the range of Cl concentrations were derived on a weight basis by plotting the calculated concentrations of Cl in the fluid …

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesOxideAnalytical chemistrychemistry.chemical_elementMineralogyBasaltic melt010502 geochemistry & geophysics01 natural sciencesChloridechemistry.chemical_compoundGeochemistry and PetrologyCl solubilityChlorinemedicine[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyFugacity0105 earth and related environmental sciencesBasalthalogen degassingGeologySilicateSettore GEO/08 - Geochimica E VulcanologiaPartition coefficientBrinechemistry13. Climate actionFluid/melt partitioningMount EtnaChlorineGeologymedicine.drug
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Evidence of organic contamination in urban soils of Cotonou town (Benin).

2012

14 pages; International audience; In Cotonou (Benin), growth of the population leads to an excessive use of natural resources, inducing organic contaminations. Surface soils collected in the town, were extracted and fractionated by liquid chromatography in three families: aliphatic, aromatic hydrocarbons and polar fractions. Each fraction was characterized by gas chromatography-mass spectrometry. All the results show that an anthropogenic input exists (waste oils). Indeed, aliphatic hydrocarbons have specific markers emphasizing the presence of petrogenic products: UCM (unresolved complex mixture), specific distribution of pentacyclic triterpane. However, specific molecular biomarkers revea…

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesPopulation[ SDV.SA.SDS ] Life Sciences [q-bio]/Agricultural sciences/Soil study010501 environmental sciences[SDV.SA.SDS]Life Sciences [q-bio]/Agricultural sciences/Soil study01 natural scienceschemistry.chemical_compound[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/GeochemistryOrganic matterpolar fractions[SDV.SA.SDS] Life Sciences [q-bio]/Agricultural sciences/Soil studyeducation0105 earth and related environmental scienceschemistry.chemical_classificationeducation.field_of_studyChemistrybiomarkersSoil classificationContamination[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistrySoil contamination[SDE.MCG] Environmental Sciences/Global ChangesPsychiatry and Mental health[ SDE.MCG ] Environmental Sciences/Global ChangesUnresolved complex mixture13. Climate actionEnvironmental chemistrySoil waterPetroleumSoilsaliphatic hydrocarbons
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Simulating future trends in hydrological regime of a large Sudano-Sahelian catchment under climate change

2012

Summary This paper assesses the future variability of water resources in the short, medium and long terms over a large Sudano-Sahelian catchment in West Africa. Flow simulations were performed with a daily conceptual model. A period of nearly 50 years (1952–2000) was chosen to capture long-term hydro-climatic variability. Calibration and validation were performed on the basis of a multi-objective function that aggregates a variety of goodness-of-fit indices. The climate models HadCM3 and MPI-M under SRES-A2 were used to provide future climate scenarios over the catchment. Outputs from these models were used to generate daily rainfall and temperature series for the 21st century according to:…

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global Changeshydro-climatic variability climatic scenarios hydrological modeling River Bani West Africa0207 environmental engineeringClimate changeRiver Bani02 engineering and technologyStructural basinHydrological modeling01 natural sciencesHadCM3EvapotranspirationWest Africa020701 environmental engineeringHydro-climatic variability0105 earth and related environmental sciencesWater Science and TechnologyClimatic scenarios6. Clean waterWater resources[ SDE.MCG ] Environmental Sciences/Global Changes[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology13. Climate actionClimatologyEnvironmental scienceClimate model[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologySurface runoffDownscalingJournal of Hydrology
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Soil moisture modelling of a SMOS pixel: interest of using the PERSIANN database over the Valencia Anchor Station

2010

In the framework of Soil Moisture and Ocean Salinity (SMOS) Calibration/Validation (Cal/Val) activities, this study addresses the use of the PERSIANN-CCS<sup>1</sup>database in hydrological applications to accurately simulate a whole SMOS pixel by representing the spatial and temporal heterogeneity of the soil moisture fields over a wide area (50×50 km<sup>2</sup>). The study focuses on the Valencia Anchor Station (VAS) experimental site, in Spain, which is one of the main SMOS Cal/Val sites in Europe. <br><br> A faithful representation of the soil moisture distribution at SMOS pixel scale (50×50 km<sup>2</sup>) requires an accurate estimation…

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global Changessatellite0207 environmental engineeringContext (language use)02 engineering and technologysystemcomputer.software_genrerainfall estimation01 natural scienceslcsh:Technologylcsh:TD1-1066Precipitation[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrologylcsh:Environmental technology. Sanitary engineering020701 environmental engineeringWater contentprecipitation estimationretrievallcsh:Environmental sciences0105 earth and related environmental sciencesRemote sensinglcsh:GE1-350DatabaseRain gaugeMoisturelcsh:Tlcsh:Geography. Anthropology. RecreationLife Sciencesneural-network15. Life on landparameterizationokavango riverproductsafricalcsh:G13. Climate actionSoil waterPERSIANNEnvironmental scienceSpatial variabilitycomputerHydrology and Earth System Sciences
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The influence of rock heterogeneity on the scaling properties of simulated and natural stylolites

2009

International audience; Stylolites are among the most prominent deformation patterns in sedimentary rocks that document localized pressure solution. Recent studies revealed that stylolite roughness is characterized by two distinct scaling regimes. The main goal of the present study is to decipher whether this complex scaling behavior of stylolites is caused by the composition of the host-rock, i.e. heterogeneities in the material, or is governed by inherent processes on respective scales, namely the transition from a surface energy to an elastic energy dominated regime, as theoretically predicted. For this purpose we have developed a discrete numerical technique, based on a lattice spring m…

010504 meteorology & atmospheric sciences[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]CompactionCompaction[SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/Petrography[SDU.STU]Sciences of the Universe [physics]/Earth SciencesSurface finish010502 geochemistry & geophysics01 natural sciencesScalingPhysics::Geophysics[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryGeotechnical engineering[PHYS.COND.CM-SM]Physics [physics]/Condensed Matter [cond-mat]/Statistical Mechanics [cond-mat.stat-mech]ScalingComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesQuenched noiseElastic energyGeologyMechanicsRoughnessSurface energyPressure solution13. Climate action[SDU]Sciences of the Universe [physics]StyloliteFinite strain theoryStylolitePressure solutionGeology
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