Search results for "climate"

showing 10 items of 4934 documents

Modelling soil moisture at SMOS scale by use of a SVAT model over the Valencia Anchor Station

2010

16 páginas, 9 figuras, 5 tablas.

010504 meteorology & atmospheric sciencestélédétectionMISSION SMOS0211 other engineering and technologiesSpaceespagne02 engineering and technologylcsh:Technology01 natural sciencesValidationTraitement du signal et de l'imagelcsh:Environmental technology. Sanitary engineering020701 environmental engineeringWater contentlcsh:Environmental sciencesComputingMilieux_MISCELLANEOUSlcsh:GE1-350InclusionRetrievalMoistureModelling soil moistureSignal and Image processinglcsh:Geography. Anthropology. RecreationRemote sensingDISPOSITIF EXPERIMENTAL; MISSION SMOSProductseurope[SPI.SIGNAL]Engineering Sciences [physics]/Signal and Image processingSMOS[SDE.MCG]Environmental Sciences/Global Changessatellite0207 environmental engineeringGrowing seasonParameterizationSpatial distributionlcsh:TD1-1066SchemeHapexspectroradiomètre14. Life underwater[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology021101 geological & geomatics engineering0105 earth and related environmental sciencesRemote sensingRadiometerlcsh:TAMSR-Epays méditerranéenSalinityERS scatterometerlcsh:G13. Climate actionDISPOSITIF EXPERIMENTALSoil waterEnvironmental scienceRadiometry
researchProduct

Mercury emissions from soils and fumaroles of Nea Kameni volcanic centre, Santorini (Greece)

2013

There have been limited studies to date targeting mercury emissions from volcanic fumarolic systems, and no mercury flux data exist for soil or fumarolic emissions at Santorini volcanic complex, Greece. We present results from the first geochemical survey of Hg and major volatile (CO2, H2S, H2O and H-2) concentrations and fluxes in the fumarolic gases released by the volcanic/hydrothermal system of Nea Kameni islet; the active volcanic center of Santorini. These data were obtained using a portable mercury spectrometer (Lumex 915+) for gaseous elemental mercury (GEM) determination, and a Multi-component Gas Analyzer System (Multi-GAS) for major volatiles. Gaseous Elemental Mercury (GEM) conc…

010504 meteorology & atmospheric sciencesvolcanogenic mercury volcanic degassing Santorini mercury flux inventory trace metalsEarth sciencetrace metalsAir pollutionchemistry.chemical_element010502 geochemistry & geophysicsmedicine.disease_cause01 natural scienceschemistry.chemical_compoundGeochemistry and Petrologymercury flux inventorymedicinevolcanogenic mercuryAir quality index0105 earth and related environmental sciencesgeographySantorinigeography.geographical_feature_categoryFumaroleSettore GEO/08 - Geochimica E VulcanologiaMercury (element)GeophysicschemistryVolcano13. Climate actionEnvironmental chemistryCarbon dioxideSoil watervolcanic degassingGeologyGEOCHEMICAL JOURNAL
researchProduct

Predicted temperature-increase-induced global health burden and its regional variability

2019

An increase in the global health burden of temperature was projected for 459 locations in 28 countries worldwide under four representative concentration pathway scenarios until 2099. We determined that the amount of temperature increase for each 100 ppm increase in global CO2 concentrations is nearly constant, regardless of climate scenarios. The overall average temperature increase during 2010–2099 is largest in Canada (1.16 °C/100 ppm) and Finland (1.14 °C/100 ppm), while it is smallest in Ireland (0.62 °C/100 ppm) and Argentina (0.63 °C/100 ppm). In addition, for each 1 °C temperature increase, the amount of excess mortality is increased largely in tropical countries such as Vietnam (10.…

010504 meteorology & atmospheric sciencesvulnerabilityVulnerabilityHot temperatureprojection010501 environmental sciencesGlobal Health01 natural sciencesGlobal WarmingRegional variationHot TemperatureAnimal scienceElderly populationPhysical Sciences and MathematicsGlobal healthHumansClimate changeProjectionMortalitylcsh:Environmental sciences0105 earth and related environmental sciencesGeneral Environmental Sciencelcsh:GE1-350Excess mortalityTemperatureregional variationPublic Health Global Health Social Medicine and EpidemiologyAtmospheric temperature rangemortality3. Good healthFolkhälsovetenskap global hälsa socialmedicin och epidemiologiclimate changeRegional variationAvaliação do Impacte em Saúde13. Climate actionEnvironmental scienceDeterminantes da Saúde e da DoençaForecasting
researchProduct

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
researchProduct

In situ carbon and oxygen isotopes measurements in carbonates by fiber coupled laser diode-induced calcination: A step towards field isotopic charact…

2021

International audience; Natural stable isotopes ratios (δ13Ccarb and δ18Ocarb) of carbonates archived in the geological record are routinely used to reconstruct local and global paleo temperatures and the secular evolution of the biogeochemical carbon cycle. The state-of-the-art technique, employed since the mid 20th century, to measure these isotopic ratios starts with field sampling followed by several steps of physical and chemical laboratory preparation including: (i) microdrilling and/or sawing and crushing, (ii) CO2 release by wet acid digestion, (iii) gas equilibration, purification and transfer, before (iv) gas phase IRMS measurements. While these steps are time and resource consumi…

010504 meteorology & atmospheric sciencesδ18OCarbonate mineralsAnalytical chemistryCarbonateschemistry.chemical_elementLaser010502 geochemistry & geophysics01 natural scienceslaw.inventionchemistry.chemical_compoundSideriteGeochemistry and Petrologylaw[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryCalcination0105 earth and related environmental sciencesCarbon isotopesGeologyCarbon cycleCalcium carbonatechemistry13. Climate actionCarbon dioxideOxygen isotopesCarbonateCarbonGeology
researchProduct

A global palaeoclimatic reconstruction for the Valanginian based on clay mineralogical and geochemical data

2020

International audience; High-resolution clay mineral and δ18Ocarb analyses have been performed on three sections of Valanginian age (Early Cretaceous), from northwestern (~20–30°N) and southern (~53°S) Tethyan realms. The data have been integrated in a large set of published mineralogical (clays), and geochemical (δ18Ocarb, δ18Obivalve, δ18Olenticulina, δ18Obelemnite, and TEX86) data from 17 sections, situated between ~45°N and ~53°S. Based on this data set, we provide new insights into Valanginian climate conditions from a wide range of palaeolatitudes. We highlight climate trends within specific areas and identify main climate belts. In the Proto-North Atlantic realm (~15–17°N) large amou…

010504 meteorology & atmospheric sciencesδ18OGlobal warming[SDU.STU]Sciences of the Universe [physics]/Earth SciencesTEX86Subtropics15. Life on land010502 geochemistry & geophysics01 natural sciencesCretaceousPaleontology13. Climate action[SDU]Sciences of the Universe [physics]General Earth and Planetary SciencesSedimentary rockThermohaline circulationGlobal coolingGeology0105 earth and related environmental sciences
researchProduct

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
researchProduct

Insolation cycles as a major control equatorial Indian Ocean primary production

1997

Analysis of a continuous sedimentary record taken in the Maldives indicates that strong primary production fluctuations (70 to 390 grams of carbon per square meter per year) have occurred in the equatorial Indian Ocean during the past 910,000 years. The record of primary production is coherent and in phase with the February equatorial insolation, whereas it shows diverse phase behavior with δ 18 O, depending on the orbital frequency (eccentricity, obliquity, or precession) examined. These observations imply a direct control of productivity in the equatorial oceanic system by insolation. In the equatorial Indian Ocean, productivity is driven by the wind intensity of westerlies, which is rel…

010504 meteorology & atmospheric sciencesδ18Omedia_common.quotation_subject[SDU.STU]Sciences of the Universe [physics]/Earth SciencesForcing (mathematics)010502 geochemistry & geophysics01 natural sciencesPhysics::Geophysics100000-year problem14. Life underwaterEccentricity (behavior)Physics::Atmospheric and Oceanic Physics0105 earth and related environmental sciencesmedia_common[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereMultidisciplinaryEquatorial wavesWesterliesOceanographyProductivity (ecology)13. Climate action[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologyClimatologyPhysics::Space PhysicsPrecessionAstrophysics::Earth and Planetary Astrophysics[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
researchProduct

A sea surface temperature reconstruction for the southern Indian Ocean trade wind belt from corals in Rodrigues Island (19°S, 63°E)

2016

Abstract. The western Indian Ocean has been warming rapidly over recent decades, causing a greater number of extreme climatic events. It is therefore of paramount importance to improve our understanding of links between Indian Ocean sea surface temperature (SST) variability, climate change and sustainability of tropical coral reef ecosystems. Here we present monthly resolved coral Sr ∕ Ca records from two different locations from Rodrigues Island (63° E, 19° S) in the south-central Indian Ocean trade wind belt. We reconstruct SST based on a linear relationship with the Sr ∕ Ca proxy with records starting from 1781 and 1945, respectively. We assess relationships between the observed long-ter…

010506 paleontology010504 meteorology & atmospheric sciences550Corallcsh:LifeClimate changeMonsoon010502 geochemistry & geophysics01 natural sciencesddc:570lcsh:QH540-549.514. Life underwaterEcology Evolution Behavior and SystematicsEarth-Surface Processes0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorySubtropical Indian Ocean Dipolelcsh:QE1-996.5Coral reeflcsh:GeologySea surface temperaturelcsh:QH501-531Oceanography13. Climate actionClimatologyIndian Ocean Dipolelcsh:EcologyGeologyTeleconnection
researchProduct

Multi-centennial summer and winter precipitation variability in southern South America

2010

[1] We present the first spatially and temporally highly resolved gridded reconstruction of multi-centennial precipitation variability for southern South America (SSA). A novel reconstruction approach of deriving 10,000 ensemble members based on varying predictor networks and methodological settings allows the identification of spatiotemporal changes in SSA precipitation and associated uncertainties. The summer and winter reconstructions back to AD 1498 and AD 1590, respectively, provide new evidence for multi-centennial increase in summer precipitation and an opposing decrease in winter precipitation into the 20th century. The drying in winter is significant over large parts of SSA, wherea…

010506 paleontology010504 meteorology & atmospheric sciencesClimate changeSeasonalityAdaptation strategiesmedicine.disease01 natural sciencesGeophysicsCentennialConvective rainfall13. Climate actionClimatologymedicineGeneral Earth and Planetary SciencesEnvironmental scienceSpatial variabilityPrecipitation0105 earth and related environmental sciencesGeophysical Research Letters
researchProduct