Search results for " RATIO"

showing 10 items of 3859 documents

Geographic and temporal variations in turbulent heat loss from lakes : A global analysis across 45 lakes

2018

Heat fluxes at the lake surface play an integral part in determining the energy budget and thermal structure in lakes, including regulating how lakes respond to climate change. We explore patterns in turbulent heat fluxes, which vary across temporal and spatial scales, using in situ high-frequency monitoring data from 45 glob- ally distributed lakes. Our analysis demonstrates that some of the lakes studied follow a marked seasonal cycle in their turbulent surface fluxes and that turbulent heat loss is highest in larger lakes and those situated at low latitude. The Bowen ratio, which is the ratio of mean sensible to mean latent heat fluxes, is smaller at low lati- tudes and, in turn, the rel…

010504 meteorology & atmospheric sciences0208 environmental biotechnologyta1172ta1171Climate change02 engineering and technologyAquatic ScienceOceanographyAtmospheric sciences01 natural sciencesjärvetLatitudeWater balanceheat fluxesLatent heatparasitic diseaseslakesBowen ratioturbulent heat loss0105 earth and related environmental sciencesthermal structurelake surface15. Life on landilmastonmuutoksetEnergy budget020801 environmental engineeringclimate change13. Climate actionHeat transferarticlesEnvironmental scienceSpatial variabilitylämpötilaenergy budgetlämpöhäviöLimnology and Oceanography
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Associations between air pollution and pediatric eczema, rhinoconjunctivitis and asthma: A meta-analysis of European birth cohorts

2020

Background: Uncertainly continues to exist regarding the role of air pollution on pediatric asthma and allergic conditions, especially as air pollution levels have started to decrease in recent decades. Objective: We examined associations of long-term air pollution levels at the home address with pediatric eczema, rhinoconjunctivitis and asthma prevalences in five birth cohorts (BIB, EDEN, GASPII, RHEA and INMA) from seven areas in five European countries. Methods: Current eczema, rhinoconjunctivitis and asthma were assessed in children aged four (N = 6527) and eight years (N = 2489). A multi-morbidity outcome (≥2 conditions versus none) was also defined. Individual outdoor levels of nitrog…

010504 meteorology & atmospheric sciencesAir pollution exposureAir pollutionEczemacross-sectional studies010501 environmental sciencesmedicine.disease_cause01 natural sciences[SDV.MHEP.PSR]Life Sciences [q-bio]/Human health and pathology/Pulmonology and respiratory tractRhinoconjunctivitisEnvironmental healthAir PollutionmedicineAir Pollutants/toxicityHumans[SDV.IMM.ALL]Life Sciences [q-bio]/Immunology/AllergologyAdverse effectChildlcsh:Environmental sciences0105 earth and related environmental sciencesGeneral Environmental ScienceAsthmaRhinitislcsh:GE1-350Pediatric[SDV.EE.SANT]Life Sciences [q-bio]/Ecology environment/Health[SDV.MHEP.PED]Life Sciences [q-bio]/Human health and pathology/PediatricsAir PollutantsOdds ratioEnvironmental Exposuremedicine.diseaseConjunctivitisConfidence intervalAsthma3. Good healthEurope13. Climate actionMeta-analysis[SDV.SPEE]Life Sciences [q-bio]/Santé publique et épidémiologieParticulate MatterConjunctivitis/epidemiologyBirth cohortEnvironmental SciencesBirth cohort
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Diagenetic stability of non-traditional stable isotope systems (Ca, Sr, Mg, Zn) in teeth – An in-vitro alteration experiment of biogenic apatite in i…

2021

Stable isotope ratios and trace element concentrations of fossil bones and teeth are important geochemical proxies for the reconstruction of diet and past environment in archaeology and palaeontology. However, since diagenesis can significantly alter primary diet-related isotope signatures and elemental compositions, it is important to understand and quantify alteration processes. Here, we present the results of in-vitro alteration experiments of dental tissues from a modern African elephant molar reacted in aqueous solutions at 30 °C and 90 °C for 4 to 63 days. Dental cubes with ≈ 3 mm edge length, comprising both enamel and dentin, were placed into 2 mL of acidic aqueous sol…

010504 meteorology & atmospheric sciencesAnalytical chemistry010502 geochemistry & geophysics01 natural sciencesApatiteDiagenesischemistry.chemical_compoundstomatognathic systemIsotopesGeochemistry and PetrologyDentinmedicineBioapatite0105 earth and related environmental sciencesIsotopeEnamel paintStable isotope ratioTrace elementLA-(MC-)ICP-MSGeologyHydroxylapatitestomatognathic diseasesmedicine.anatomical_structurechemistry13. Climate actionvisual_artRaman spectroscopyvisual_art.visual_art_mediumEPMAGeologyEMPA
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Intra- and inter-annual uranium concentration variability in a Belizean stalagmite controlled by prior aragonite precipitation: A new tool for recons…

2016

Aragonitic speleothems are increasingly utilised as palaeoclimate archives due to their amenability to high precision U–Th dating. Proxy records from fast-growing aragonitic stalagmites, precisely dated to annual timescales, can allow investigation of climatic events occurring on annual or even sub-annual timescales with minimal chronological uncertainty. However, the behaviour of many trace elements, such as uranium, in aragonitic speleothems has not thus far been as well constrained as in calcitic speleothems. Here, we use uranium concentration shifts measured across primary calcite-to-aragonite mineralogical transitions in speleothems to calculate the distribution coefficient of uranium …

010504 meteorology & atmospheric sciencesGeochemistryF700MineralogySpeleothemF800StalagmiteF600engineering.material010502 geochemistry & geophysics01 natural sciencesF900Geochemistry and PetrologymedicinePrecipitation0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryδ13CStable isotope ratioAragoniteTrace element15. Life on landSeasonalitymedicine.disease13. Climate actionengineeringGeologyGeochimica et Cosmochimica Acta
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Sr/Ca and Mg/Ca ratios of ontogenetically old, long-lived bivalve shells (Arctica islandica) and their function as paleotemperature proxies

2011

International audience; The Sr/Ca and Mg/Ca ratios of many biogenic skeletons provide useful paleotemperature estimates. As yet however, it has remained largely impossible to obtain such information from bivalve shells. In the present study, metal-to-calcium values in the hinge plate (aragonite, outer shell layer) of four ontogenetically old (85 to 374 year-old) specimens of the long-lived bivalve, Arctica islandica, were measured on a LA-ICP-MS. The shells were collected alive in 1868, 1986 and 2003 from three different localities around Iceland. With increasing ontogenetic age and decreasing growth rate, a distinct trend toward increasing Sr/Ca (max. 5.17 mmol/mol) and Mg/Ca values (max. …

010504 meteorology & atmospheric sciencesOntogenySea surface temperatureLongevityZoologyMineralogyAmbient waterengineering.materialSignificant negative correlation010502 geochemistry & geophysicsOceanography01 natural sciencesMetal-to-calcium ratioMole14. Life underwaterGrowth rateBivalve shellArctica islandicaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesVital effectbiologyAragonitePaleontologybiology.organism_classificationBivalve shell[SDE]Environmental Sciencesengineering
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Identification of processes that control the stable isotope composition of rainwater in the humid tropical West-Central Africa.

2020

12 pages; International audience; This study interprets 11 years (2006 to 2016) and 6 months (March to August in 2017) of respectively monthly and daily isotopic (δD and δ18O) monitoring of rain at Douala (Cameroon), a humid tropical station in Western Africa. The main scope is to analyze the climate controls on precipitation isotopes at different timescales. Firstly, we examine the annual cycles of δ18O. Over the 11 years of survey, the annual cycle exhibits a W shape that is quite reproducible from year to year, with two minima in spring and autumn periods. Based on back trajectory calculations and remote sensing observations of water vapor isotopic composition, we show that the observed …

010504 meteorology & atmospheric sciencesδ18O0207 environmental engineeringHumid subtropical climate02 engineering and technologyAtmospheric sciencesAir back trajectory01 natural sciencesGPCP precipitation[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistrySpring (hydrology)Precipitation020701 environmental engineeringδ18OComputingMilieux_MISCELLANEOUSAir mass0105 earth and related environmental sciencesWater Science and TechnologyWater vapor[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmospheregeographygeography.geographical_feature_categoryStable isotope ratioAnnual cycleConvective activity[SDU]Sciences of the Universe [physics]13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyEnvironmental scienceWater vapor
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Simulating speleothem growth in the laboratory: Determination of the stable isotope fractionation (δ13C and δ18O) between H2O, DIC and CaCO3

2019

Abstract Here we present novel cave-analogue experiments directly investigating stable carbon and oxygen isotope fractionation between the major involved species of the carbonate system (HCO3−, CO2, CaCO3 and H2O). In these experiments, which were performed under controlled conditions inside a climate box, a thin film of solution flew down an inclined marble or glass plate. After different distances of flow and, thus, residence times on the plate, pH, electrical conductivity, supersaturation with respect to calcite, precipitation rate as well as the δ18O and δ13C values of the dissolved inorganic carbon (DIC) and the precipitated CaCO3 were obtained. Progressive precipitation of CaCO3 along…

010504 meteorology & atmospheric sciencesδ18OStable isotope ratioAnalytical chemistryGeologyFractionation010502 geochemistry & geophysics01 natural sciencesIsotopes of oxygenEquilibrium fractionationIsotope fractionation13. Climate actionGeochemistry and PetrologyIsotopes of carbonRayleigh fractionationGeology0105 earth and related environmental sciencesChemical Geology
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Oxygen isotope compositions of phosphate from arvicoline teeth and Quaternary climatic changes, Gigny, French Jura

2004

Oxygen isotope compositions of biogenic phosphates from mammals are widely used as proxies of the isotopic compositions of meteoric waters that are roughly linearly related to the air temperature at high- and mid-latitudes. An oxygen isotope fractionation equation was determined by using present-day European arvicoline (rodents) tooth phosphate: δ18Op = 20.98(±0.59) + 0.572(±0.065) δ18Ow. This fractionation equation was applied to the Late Pleistocene karstic sequence of Gigny, French Jura. Comparison between the oxygen isotope compositions of arvicoline tooth phosphate and Greenland ice core records suggests to reconsider the previously established hypothetical chronology of the sequence. …

010506 paleontology010504 meteorology & atmospheric sciencesPleistoceneGeochemistryFractionationOxygen isotope ratio cyclePhosphate01 natural sciencesIsotopes of oxygenchemistry.chemical_compoundPaleontologyArts and Humanities (miscellaneous)chemistryIce coreGeneral Earth and Planetary SciencesQuaternaryGeology0105 earth and related environmental sciencesEarth-Surface ProcessesChronologyQuaternary Research
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Carbon and oxygen stable isotope compositions of late Pleistocene mammal teeth from dolines of Ajoie (Northwestern Switzerland)

2014

AbstractFossils of megaherbivores from eight late Pleistocene 14C- and OSL-dated doline infillings of Ajoie (NW Switzerland) were discovered along the Transjurane highway in the Swiss Jura. Carbon and oxygen analyses of enamel were performed on forty-six teeth of large mammals (Equus germanicus, Mammuthus primigenius, Coelodonta antiquitatis, and Bison priscus), coming from one doline in Boncourt (~ 80 ka, marine oxygen isotope stage MIS5a) and seven in Courtedoux (51–27 ka, late MIS3), in order to reconstruct the paleoclimatic and paleoenvironmental conditions of the region. Similar enamel δ13C values for both periods, ranging from − 14.5 to − 9.2‰, indicate that the megaherbivores lived i…

010506 paleontology010504 meteorology & atmospheric sciencesPleistocenePaleoclimateRange (biology)[SDV]Life Sciences [q-bio]Tooth enamel01 natural sciencesIsotopes of oxygenPaleontologyArts and Humanities (miscellaneous)PaleoclimatologyEarly GlacialPaleodiet0105 earth and related environmental sciencesEarth-Surface ProcessesMiddle Pleniglacial[SDV.EE]Life Sciences [q-bio]/Ecology environmentbiologyEnamel paintStable isotope ratio[SDV.BA]Life Sciences [q-bio]/Animal biology15. Life on landbiology.organism_classificationEquusPaleoenvironment13. Climate actionvisual_artvisual_art.visual_art_mediumGeneral Earth and Planetary SciencesMammalGeologyMegaherbivores
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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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