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showing 10 items of 34508 documents

Secondary minerals from salt caves in the Atacama Desert (Chile): a hyperarid and hypersaline environment with potential analogies to the Martian sub…

2017

Over the past 15 years several expeditions by French, American and especially Italian cavers have unveiled over 50 caves in the Cordillera de la Sal (Atacama Desert, Northern Chile). Many of these caves contain a variety of speleothems and minerals, some of which have rarely been observed within karst systems. Most of the secondary deposits in these caves are composed of halite, but also other halide, carbonate, sulphate, nitrate, phosphate, and silicate minerals have been found. Among the sixteen cave mineral species recognized, atacamite, darapskite, blödite, leonite, anhydrite, and especially antarcticite are worth mentioning. In one of the samples an unknown Ca-Sr-bearing chloride miner…

010504 meteorology & atmospheric sciencesQH301-705.5Settore GEO/04 - Geografia Fisica E GeomorfologiaEarth scienceSalt (chemistry)martian010502 geochemistry & geophysics01 natural sciencesAstrobiologyatacamaCaveminerogenesisMinerogenesiBiology (General)Hyperaridity0105 earth and related environmental sciencesEarth-Surface Processescave mineralschemistry.chemical_classificationMartianQE1-996.5Settore GEO/06 - Mineralogiageographygeography.geographical_feature_categoryDesert (philosophy)Mars analoguesMars analogueCave mineralGeologysalt cavescave minerals atacama martianchemistrySalt cavecave minerals salt caves hyperaridity minerogenesis Mars analoguesGeologyInternational Journal of Speleology
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Potential-vorticity dynamics of troughs and ridges within Rossby wave packets during a 40-year reanalysis period

2020

Rossby wave packets (RWPs) are fundamental to midlatitude dynamics and govern weather systems from their individual life cycles to their climatological distributions. Renewed interest in RWPs as precursors to high-impact weather events and in the context of atmospheric predictability motivates this study to revisit the dynamics of RWPs. A quantitative potential vorticity (PV) framework is employed. Based on the well established PV-thinking of midlatitude dynamics, the processes governing RWP amplitude evolution comprise group propagation of Rossby waves, baroclinic interaction, the impact of upper-tropospheric divergent flow, and direct diabatic PV modification by nonconservative processes.…

010504 meteorology & atmospheric sciencesRadiative coolingBaroclinityRossby waveContext (language use)010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesInstabilityPotential vorticityLatent heatBarotropic fluidMeteorology. ClimatologyQC851-999Geology0105 earth and related environmental sciencesWeather and Climate Dynamics
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A process-based anatomy of Mediterranean cyclones: from baroclinic lows to tropical-like systems

2021

Abstract. In this study, we address the question of the atmospheric processes that turn Mediterranean cyclones into severe storms. Our approach applies on-line potential vorticity (PV) budget diagnostics and piecewise PV inversion to WRF model simulations of the mature stage of 100 intense Mediterranean cyclones. We quantify the relative contributions of different processes to cyclone development and therefore deliver, for the first time, a comprehensive insight into the variety of cyclonic systems that develop in the Mediterranean from the perspective of cyclone dynamics. In particular, we show that all 100 cyclones are systematically influenced by two main PV anomalies: a major anomaly in…

010504 meteorology & atmospheric sciencesRadiative coolingSevere weatherBaroclinity0208 environmental biotechnologyDiabatic02 engineering and technology01 natural sciences020801 environmental engineeringTroposphere13. Climate actionMeteorology. ClimatologyClimatologyLatent heatWeather Research and Forecasting ModelCycloneEnvironmental scienceQC851-9990105 earth and related environmental sciencesWeather and Climate Dynamics
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Hydrological drivers of wetland vegetation community distribution within Everglades National Park, Florida

2010

The influence of hydrological dynamics on vegetation distribution and the structuring of wetland environments is of growing interest as wetlands are modified by human action and the increasing threat from climate change. Hydrological properties have long been considered a driving force in structuring wetland communities. We link hydrological dynamics with vegetation distribution across Everglades National Park (ENP) using two publicly available datasets to study the probability structure of the frequency, duration, and depth of inundation events along with their relationship to vegetation distribution. This study is among the first to show hydrologic structuring of vegetation communities at…

010504 meteorology & atmospheric sciencesRange (biology)Climate changeWetland010501 environmental sciences01 natural sciencesModelsVegetation typeValidationLandscapeTemporal scales0105 earth and related environmental sciencesWater Science and TechnologyHydrologyEverglades Vegetation Hydrology Wetlandsgeographygeography.geographical_feature_categoryVegetationNational parkSettore ICAR/02 - Costruzioni Idrauliche E Marittime E IdrologiaCommunity structureVegetation15. Life on landEvergladesScale13. Climate actionWetlandsEnvironmental scienceHydrology
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Validation of a novel Multi-Gas sensor for volcanic HCl alongside H2S and SO2 at Mt. Etna

2017

Erratum to: Bull Volcanol (2017) 79: 36DOI 10.1007/s00445-017-1114-zDuring the steps of corrections, the publisher inadvertently changed the author affiliations so that they were no longer correct. The correct information is given below. The publisher regrets this mistake.; International audience; Volcanic gas emission measurements inform predictions of hazard and atmospheric impacts. For these measurements, Multi-Gas sensors provide low-cost in situ monitoring of gas composition but to date have lacked the ability to detect halogens. Here, two Multi-Gas instruments characterized passive outgassing emissions from Mt. Etna’s (Italy) three summit craters, Voragine (VOR), North-east Crater (NE…

010504 meteorology & atmospheric sciencesResponse modelPoison controlMineralogyOpen-system volcanic degassing010502 geochemistry & geophysics01 natural sciencesElectronic noseImpact craterGeochemistry and PetrologyCalibrationGas compositionVolcanic outgassing0105 earth and related environmental sciencesMulti-Gas instrumentgeographygeography.geographical_feature_categoryE-noseOutgassingVolcano13. Climate action[SDU]Sciences of the Universe [physics]HalogenMagmaChlorineGeology
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Spatial variability of the relationships of runoff and sediment yield with weather types throughout the Mediterranean basin

2019

Este artículo contiene 16 páginas, 6 figuras, 2 tablas.

010504 meteorology & atmospheric sciencesRunoffErosion; Mediterranean basin; Runoff; Sediment yield; Synoptic weather types0207 environmental engineering[SDU.STU]Sciences of the Universe [physics]/Earth Sciences02 engineering and technology01 natural sciencesMediterranean BasinHydrology (agriculture)Erosão Produção de sedimentos Escoamento Bacia MediterrânicaSoil retrogression and degradationddc:550020701 environmental engineering0105 earth and related environmental sciencesWater Science and TechnologyHydrologyMediterranean basinSediment yieldSedimentInstitut für Umweltwissenschaften und Geographie15. Life on land6. Clean waterSynoptic weather typesErosion13. Climate actionErosion; Mediterranean basin; Runoff; Sediment yield; Synoptic weather types; Water Science and TechnologyErosionEnvironmental scienceSpatial variabilitySoil conservationSurface runoff
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Late Quaternary Variations in the South American Monsoon System as Inferred by Speleothems—New Perspectives using the SISAL Database

2019

Here we present an overview of speleothem δ18O records from South America, most of which are available in the Speleothem Isotopes Synthesis and Analysis (SISAL_v1) database. South American tropical and subtropical speleothem δ18O time series are primarily interpreted to reflect changes in precipitation amount, the amount effect, and consequently history of convection intensity variability of convergence zones such as the Intertropical Convergence Zone (ITCZ) and the South America Monsoon System (SAMS). We investigate past hydroclimate scenarios in South America related to the South American Monsoon System in three different time periods: Late Pleistocene, Holocene, and the last tw…

010504 meteorology & atmospheric sciencesSAMSSpeleothemlcsh:GN281-289SubtropicsSouth American Monsoon System010502 geochemistry & geophysicscomputer.software_genreMonsoon01 natural scienceslcsh:StratigraphyEarth and Planetary Sciences (miscellaneous)PrecipitationSISALHolocenelcsh:QE640-6990105 earth and related environmental sciencesEarth-Surface Processesgeographyquaternarygeography.geographical_feature_categoryDatabasespeleothemsIntertropical Convergence ZoneMUDANÇA CLIMÁTICAlcsh:Human evolutionSouth Atlantic Convergence ZoneQuaternarycomputerGeologyQuaternary
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Cretaceous ultrapotassic magmatism from the Sava-Vardar Zone of the Balkans

2020

Highlights • Geochemically diverse Late Cretaceous small-volume magmatism in the Sava-Vardar Zone. • Late Cretaceous ultrapotassic lava, equivalent of minette and kersantite. • Magma derivation from a LREE and K enriched, garnet-bearing anciently metasomatized mantle source. • Magmatism occurred either in a fore-arc setting or is associated with transtensional tectonics. Abstract Late Cretaceous global plate reorganization associated with the inception of counterclockwise rotation of Africa relative to Europe initiated in the Balkan region small-volume magmatism of diverse geochemical signature along the enigmatic Sava-Vardar Zone. We study a Late Cretaceous lamprophyric sill in Ripanj vill…

010504 meteorology & atmospheric sciencesSava-Vardar zoneGeochemistryengineering.material010502 geochemistry & geophysicsFeldspar01 natural sciencesMantle (geology)Cretaceous ultrapotassic rocksSillGeochemistry and PetrologySava-Vardar zonaMesozoic0105 earth and related environmental sciencesMantle metasomatismgeographygeography.geographical_feature_categorySubductionKredne ultrakalijske steneGeologyDurbachite-vaugnerite serijaReconstruction geochemistryCretaceousDurbachite-vaugnerite series13. Climate actionvisual_artMagmatismengineeringvisual_art.visual_art_mediumPhlogopiteGeologymetasomatizam omotača
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Transboundary Basins Need More Attention: Anthropogenic Impacts on Land Cover Changes in Aras River Basin, Monitoring and Prediction.

2020

Changes in land cover (LC) can alter the basin hydrology by affecting the evaporation, infiltration, and surface and subsurface flow processes, and ultimately affect river water quantity and quality. This study aimed to monitor and predict the LC composition of a major, transboundary basin contributing to the Caspian Sea, the Aras River Basin (ARB). To this end, four LC maps of ARB corresponding to the years 1984, 2000, 2010, and 2017 were generated using Landsat satellite imagery from Armenia and the Nakhchivan Autonomous Republic. The LC gains and losses, net changes, exchanges, and the spatial trend of changes over 33 years (1984–2017) were investigated. The most important drivers of the…

010504 meteorology & atmospheric sciencesScienceDrainage basinland change modelerLand cover010501 environmental sciencesStructural basin01 natural sciencesremote sensingHydrology (agriculture)Satellite imagerySubsurface flow0105 earth and related environmental sciences2. Zero hungergeographygeography.geographical_feature_categorybusiness.industryQ15. Life on land6. Clean wateranthropogenic impactsWater resourcesAras River Basin13. Climate actionAgriculturetransboundary basinGeneral Earth and Planetary SciencesEnvironmental scienceWater resource managementbusinessRemote sensing
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Magmas near the critical degassing pressure drive volcanic unrest towards a critical state

2016

During the reawaking of a volcano, magmas migrating through the shallow crust have to pass through hydrothermal fluids and rocks. The resulting magma–hydrothermal interactions are still poorly understood, which impairs the ability to interpret volcano monitoring signals and perform hazard assessments. Here we use the results of physical and volatile saturation models to demonstrate that magmatic volatiles released by decompressing magmas at a critical degassing pressure (CDP) can drive volcanic unrest towards a critical state. We show that, at the CDP, the abrupt and voluminous release of H2O-rich magmatic gases can heat hydrothermal fluids and rocks, triggering an accelerating deformation …

010504 meteorology & atmospheric sciencesScienceGeneral Physics and AstronomyPoison control010502 geochemistry & geophysics01 natural sciencesGeneral Biochemistry Genetics and Molecular BiologyHydrothermal circulationArticlePhysics and Astronomy (all)PetrologyVolcanic unrest0105 earth and related environmental sciencesgeographyMultidisciplinarygeography.geographical_feature_categoryBiochemistry Genetics and Molecular Biology (all)QChemistry (all)CrustGeneral ChemistryPhysics and Astronomy (all) Volcano Eruption Unrest Campi FlegreiVolcano13. Climate actionMagmaRock failureGeologyPressure.drive
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