Search results for "CLIMATE"

showing 10 items of 4934 documents

Climate change: A driver of future conflicts in the Persian Gulf Region?

2021

Ongoing global change and its direct environmental impacts, in addition to securing economic transition to the post-oil era, could trigger complex socio-economic and political crises in oil-dependent economies of the Persian Gulf Region (PGR). To evaluate the role of climate change and related policies in degrading the environment and its socio-economic impacts in the PGR, we have used a variety of available global datasets and published data. The results show that the countries of the PGR pursue some types of socio-economic reforms to alleviate the impacts of climate change. However, it seems that these attempts are not compatible with the environment's capacity. The main problem stems fro…

010504 meteorology & atmospheric sciencesWater scarcityPersian GulfClimate change010501 environmental sciencesEnvironmentCollective actionGeopolitics01 natural sciencesWater scarcityEffects of global warming11. SustainabilityDevelopment economicsRevenueClimate changelcsh:Social sciences (General)lcsh:Science (General)0105 earth and related environmental sciencesMultidisciplinary1. No povertyGlobal changeEconomy13. Climate actionPreparedness8. Economic growth[SDE]Environmental Scienceslcsh:H1-99BusinessResearch Articlelcsh:Q1-390Heliyon
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Global Groundwater-Vegetation Relations

2017

Groundwater is an integral component of the water cycle, and it also influences the carbon cycle by supplying moisture to ecosystems. However, the extent and determinants of groundwater-vegetation interactions are poorly understood at the global scale. Using several high-resolution data products, we show that the spatial patterns of ecosystem gross primary productivity and groundwater table depth are correlated during at least one season in more than two-thirds of the global vegetated area. Positive relationships, i.e., larger productivity under shallower groundwater table, predominate in moisture-limited dry to mesic conditions with herbaceous and shrub vegetation. Negative relationships, …

010504 meteorology & atmospheric sciencesWater table0208 environmental biotechnology02 engineering and technologyecohydrological patterns01 natural sciencesgroundwaterEcosystemWater cycleplant productivity0105 earth and related environmental sciencesHydrologyecosystemVegetation15. Life on land6. Clean water020801 environmental engineeringGeophysicsProductivity (ecology)13. Climate actionSpatial ecologyGeneral Earth and Planetary SciencesEnvironmental scienceGroundwaterWater usespatial covariation
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Results from DROXO IV. EXTraS discovery of an X-ray flare from the Class I protostar candidate ISO-Oph 85

2016

X-ray emission from Young Stellar Objects (YSOs) is crucial to understand star formation. A very limited amount of X-ray results is available for the protostellar (ClassI) phase. A systematic search of transient X-ray phenomena combined with a careful evaluation of the evolutionary stage offer a widely unexplored window to our understanding of YSOs X-ray properties. Within the EXTraS project, a search for transients and variability in the whole XMM-Newton archive, we discover transient X-ray emission consistent with ISO-Oph 85, a strongly embedded YSO in the rho Ophiuchi region, not detected in previous time-averaged X-ray studies. We extract an X-ray light curve for the flare and determine…

010504 meteorology & atmospheric sciencesYoung stellar objectAstrophysics::High Energy Astrophysical PhenomenaPopulationFOS: Physical sciencesAstrophysicsAstrophysics::Cosmology and Extragalactic Astrophysics01 natural sciencesflares; X-rayslaw.inventionPhotometry (optics)law0103 physical sciencesProtostarAstrophysics::Solar and Stellar Astrophysicseducation010303 astronomy & astrophysicsAstrophysics::Galaxy AstrophysicsSolar and Stellar Astrophysics (astro-ph.SR)0105 earth and related environmental sciencescoronaePhysicseducation.field_of_studystars: protostarsStar formationactivityAstronomy and AstrophysicsLight curveAstrophysics - Solar and Stellar Astrophysics13. Climate actionSpace and Planetary ScienceSpectral energy distributionAstrophysics::Earth and Planetary AstrophysicsFlare
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Long-term annual burning of grassland increases CO2 emissions from soils.

2016

7 pages; International audience; Grasslands have potential to mitigate against climate change because of their large capacity to store soil organic carbon (SOC). However, the long-term impact of grassland management such as burning, which is still common in many areas of the world, on SOC is still a matter of debate. The objective of this study was to quantify the long-term effects of annual burning on CO2 output from soils and SOC stocks. The study was performed on a 62 years old field trial comparing annual burning (AB) to no burning associated with tree encroachment (NB), and to annual mowing (AM) with all treatments laid out in randomized block design with three replicates per treatment…

010504 meteorology & atmospheric sciences[ SDV.SA.SDS ] Life Sciences [q-bio]/Agricultural sciences/Soil study[SDV.SA.AGRO]Life Sciences [q-bio]/Agricultural sciences/AgronomySoil Science[SDV.SA.SDS]Life Sciences [q-bio]/Agricultural sciences/Soil study01 natural sciencesCarbon cycleSoil respiration[ SDV.SA.AGRO ] Life Sciences [q-bio]/Agricultural sciences/AgronomyGrassland managementWater content0105 earth and related environmental sciences2. Zero hungerBurningSoil organic matterSoil chemistry04 agricultural and veterinary sciencesSoil carbonSoil respirationCarbon cycle15. Life on landBulk densitySoil carbonAgronomy13. Climate actionSoil water040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental science
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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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