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showing 10 items of 2807 documents

Characterization of electronic properties of the Cr(CO)3 group in chromium, tricarbonyl [3-[(η6-aryl)methylene]-Z-1(3H)-isobenzofuranones] using spec…

1999

Abstract The IR, 13C- and 17O-NMR spectral characteristics of the Cr(CO)3 group in a series of eight chromium, tricarbonyl[3-[(η6-aryl)methylene]-Z-1(3H)-isobenzofuranones] were correlated mutually as well as with theoretical data obtained by optimized MMX force-field and EHT calculations. The net charges on the carbon and oxygen atoms of the CO group and their differences were found as the most appropriate quantitative characteristics for the electronic properties of the Cr(CO)3 group. Using the results of the previously reported linear correlations, the electron-withdrawing effect of the PhCr(CO)3 moiety, weakened by the back-donation effect, was estimated as σα≅0.45 on the scale of Hamm…

ArylOrganic ChemistrySubstituentInfrared spectroscopychemistry.chemical_elementPhotochemistryBiochemistryInorganic Chemistrychemistry.chemical_compoundChromiumchemistryGroup (periodic table)Materials ChemistryPhysical chemistryMoietyPhysical and Theoretical ChemistryMethyleneCarbonJournal of Organometallic Chemistry
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Assessments for the impact of mineral dust on the meningitis incidence in West Africa.

2013

9 pages; International audience; Recently, mineral dust has been suspected to be one of the important environmental risk factor for meningitis epidemics in West Africa. The current study is one of the first which relies on long-term robust aerosol measurements in the Sahel region to investigate the possible impact of mineral dust on meningitis cases (incidence). Sunphotometer measurements, which allow to derive aerosol and humidity parameters, i.e., aerosol optical thickness, Angström coefficient, and precipitable water, are combined with quantitative epidemiological data in Niger and Mali over the 2004-2009 AMMA (African Monsoon Multidisciplinary Analysis) program period. We analyse how th…

Atmospheric Science010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesDry seasonContext (language use)010501 environmental sciencesMineral dustMonsoon01 natural sciencescomplex mixtures[SDV.MHEP.MI]Life Sciences [q-bio]/Human health and pathology/Infectious diseasesDry seasonWest AfricamedicineMeningitis0105 earth and related environmental sciencesGeneral Environmental Science2. Zero hungerPrecipitable waterHumidityDustmedicine.diseaseAerosol[ SDE.MCG ] Environmental Sciences/Global Changes[ SDV.MHEP.MI ] Life Sciences [q-bio]/Human health and pathology/Infectious diseases13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyClimatologyEnvironmental science[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/ClimatologyMeningitis
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Interannual variability of Greenland winter precipitation sources: 2. Effects of North Atlantic Oscillation variability on stable isotopes in precipi…

2008

[1] A new Lagrangian moisture source diagnostic is applied to identify the atmospheric conditions relevant for the fractionation of stable water isotopes during evaporation over the ocean and subsequent transport to Greenland. Northern Hemisphere winter months with positive and negative North Atlantic Oscillation (NAO) index are studied on the basis of ERA-40 reanalysis data. Diagnosed moisture transport conditions are supplied to a Rayleigh-type isotope fractionation model to derive estimates for the isotopic composition of stable isotopes in winter precipitation on the Greenland plateau for the two NAO phases. Because of changes in atmospheric circulation, moisture source locations for pr…

Atmospheric Science010504 meteorology & atmospheric sciencesδ18O0207 environmental engineeringSoil ScienceGreenland ice sheet02 engineering and technologyAquatic ScienceOceanography01 natural sciencesIsotope fractionationIce coreGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)020701 environmental engineering[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesWater Science and Technology[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereEcologyStable isotope ratioNorthern HemispherePaleontologyForestrySea surface temperatureGeophysics13. Climate actionSpace and Planetary ScienceNorth Atlantic oscillationClimatologyEnvironmental science
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δ13C variations in tree rings as an indication of severe changes in the urban air quality

2002

Abstract Annual growth rings sampled from three free-standing trees (Platanus hybrida sp.), grew in the metropolitan area of Palermo (Italy) and covering a 118 years time span (1880–1998), have been studied for their 13C/12C carbon isotope ratios. It has been found that the 13C/12C tree ring record, during the study time interval, decreased of −3.6‰, from −26.4‰ in 1880 to −30‰ in 1998. Such a progressive depletion has been attributed to the addition of anthropogenic 13C depleted carbon dioxide to the local atmosphere. The observed 13C/12C decrease has been used to infer some possible pathways of atmospheric CO2 change in the study urban area.

Atmospheric ScienceAir pollutionMineralogyUrban environmentAtmospheric sciencesmedicine.disease_causeAtmospherechemistry.chemical_compoundmedicineDendrochronologyEnvironmental geochemistryAir quality indexGeneral Environmental Scienceδ13Cbiologybiology.organism_classificationStable carbon isotopeSettore GEO/08 - Geochimica E VulcanologiaPlatanuschemistryCarbon dioxideIsotopes of carbonCarbon dioxideEnvironmental scienceDendrochemistryTree ring
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Paleoceanography of the Late Cretaceous northwestern Tethys Ocean: Seasonal upwelling or steady thermocline?

2020

In this study we attempted to assess whether seasonal upwelling or a steady thermocline persisted at the western margin of the Tethys Ocean during the late Turonian-early Coniacian interval. For this scope, we employed novel and published stable oxygen isotope (δ18O) data of various organisms (bivalves, bivalves, brachiopods, fish and belemnites). New seasonally resolved temperature estimates were based on the δ18O record of sequentially sampled inoceramid (Inoceramus sp.) and rudist (Hippurites resectus) shells from the Scaglia Rossa and Gosau deposits of northern Italy and western Austria, respectively. Diagenetic screening was performed using reflected light, cathodoluminescence (CL), sc…

Atmospheric ScienceComposite Particles010504 meteorology & atmospheric sciencesMarine and Aquatic SciencesOxygen IsotopesOceanography010502 geochemistry & geophysics01 natural sciencesIsotopesClimatologyCretaceous PeriodMultidisciplinarybiologyPhysicsStable IsotopesQRTemperatureEukaryotaGeologyCretaceousOceanographyPhysical SciencesMedicineMesozoic EraSeasonsPaleotemperatureGeologyResearch ArticleShallow WaterInoceramusBivalvesAtomsWater massScienceOceans and SeasPaleoenvironmentsPaleoceanographyAnimalsPaleoclimatologyParticle PhysicsOcean Temperature0105 earth and related environmental sciencesOrganismsPaleontologyWaterBiology and Life SciencesGeologic TimeMolluscsTethys Oceanbiology.organism_classificationInvertebratesBivalviaWaves and shallow waterEarth SciencesUpwellingHydrologyZoologyThermoclinePLOS ONE
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Lagrangian simulations of stable isotopes in water vapor: An evaluation of nonequilibrium fractionation in the Craig-Gordon model

2009

[1] The Craig-Gordon model is the basis for the parameterization of water isotope fractionation during evaporation from the ocean in many atmospheric isotope models. Its exact formulation (e.g., with respect to the nonequilibrium fractionation factor k) is mainly based on theoretical considerations and not very well constrained by observations. This study addresses this issue by combining a recently developed Lagrangian moisture source analysis with a Craig-Gordon fractionation parameterization for the identified evaporation events in order to model isotope ratios in water vapor. This technique is applied to 45 measurement days of isotopes in water vapor at Rehovot (Israel) during the years…

Atmospheric ScienceEcologyMeteorologyStable isotope ratioEvaporationPaleontologySoil ScienceNon-equilibrium thermodynamicsThermodynamicsForestryAquatic ScienceOceanographyWind speedGeophysicsIsotope fractionationDeuteriumSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Environmental scienceParametrizationPhysics::Atmospheric and Oceanic PhysicsWater vaporEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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Air parcel trajectory analysis of stable isotopes in water vapor in the eastern Mediterranean

2008

[1] With the help of a Lagrangian moisture source diagnostic, linkages between stable isotope measurements in water vapor in Rehovot (Israel), with typical sampling times of 8 hours, and the meteorological conditions in the evaporation regions are established. These linkages can be formulated in quantitative terms, and are also quantitatively comparable with other data from isotope measurements over the ocean and with simple theoretical calculations. On the one hand, a strong negative correlation (r = −0.82) between relative humidity with respect to sea surface temperature in the source regions and measured deuterium excess (d) is found, corroborating results from isotope global circulation…

Atmospheric ScienceEcologyMoistureMeteorologyIsotopeStable isotope ratioEvaporationPaleontologySoil ScienceForestryAquatic ScienceOceanographyAtmospheric sciencesSea surface temperatureGeophysicsMediterranean seaSpace and Planetary ScienceGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)Environmental scienceRelative humidityWater vaporEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research
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Low-frequency noise inδ13C andδ18O tree ring data: A case study ofPinus uncinatain the Spanish Pyrenees

2010

[1] Isotopic discrimination measurements in tree rings are becoming increasingly important estimators of past environmental change. Potential biases inherent to these parameters, including age trend and level offset are, however, not well understood. We here perform measurements on a new millennium-long data set of decadally resolved δ18O and δ13C discrimination from 25 high-elevation pine trees in the Spanish Pyrenees to investigate whether such low-frequency biases exist and how they alter the long-term behavior of derived time series. Alignment of the tree ring data by biological age reveals age trends over the first one to four centuries after germination. On average, isotope values cha…

Atmospheric ScienceGlobal and Planetary ChangeSeries (stratigraphy)Environmental changeδ13Cδ18OStable isotope ratioEcologyEstimatorDendrochronologyEnvironmental ChemistryPhysical geographyTree (set theory)General Environmental ScienceMathematicsGlobal Biogeochemical Cycles
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Dynamics of a local Alpine flooding event in October 2011: moisture source and large‐scale circulation

2014

Alpine heavy precipitation events often affect small catchments, although the circulation pattern leading to the event extends over the entire North Atlantic. The various scale interactions involved are particularly challenging for the numerical weather prediction of such events. Unlike previous studies focusing on the southern Alps, here a comprehensive study of a heavy precipitation event in the northern Alps in October 2011 is presented with particular focus on the role of the large-scale circulation in the North Atlantic/European region. During the event exceptionally high amounts of total precipitable water occurred in and north of the Alps. This moisture was initially transported alon…

Atmospheric ScienceOceanographyPrecipitable water13. Climate actionPotential vorticityClimatologyRossby waveRidge (meteorology)PrecipitationSubtropicsAtmospheric riverTrough (meteorology)GeologyQuarterly Journal of the Royal Meteorological Society
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Summertime columnar content of atmospheric water vapor from ground-based Sun-sky radiometer measurements through a new in situ procedure

2010

[1] A new in situ technique for the retrieval of atmospheric water vapor content (i.e., precipitable water content) from Sun photometric direct solar irradiance measurements, taken at the 940 nm wavelength during clear‐sky conditions, is presented. The procedure is applied to summer data recorded in 2007, 2008, and 2009 with a Sun‐sky radiometer at the San Pietro Capofiume station in the Po valley, Italy. It is a preliminary development of the retrieval procedure providing the columnar water vapor content from measurements performed with PREDE Sun‐sky radiometers. The technique brings improvement and innovation by retrieving the best values of constants (a and b), characterizing atmospheric…

Atmospheric ScienceSoil ScienceAquatic ScienceOceanographySolar irradiancelaw.inventionGeochemistry and PetrologylawEarth and Planetary Sciences (miscellaneous)Relative humidityWater contentEarth-Surface ProcessesWater Science and TechnologyRemote sensingRadiometerEcologyPrecipitable waterAtmospheric pressure451PaleontologyForestryGeophysicsSpace and Planetary ScienceRadiosondeEnvironmental scienceWater vaporJournal of Geophysical Research
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