Search results for "sphere"

showing 10 items of 2121 documents

Global Sensitivity Analysis of Leaf-Canopy-Atmosphere RTMs: Implications for Biophysical Variables Retrieval from Top-of-Atmosphere Radiance Data.

2019

Knowledge of key variables driving the top of the atmosphere (TOA) radiance over a vegetated surface is an important step to derive biophysical variables from TOA radiance data, e.g., as observed by an optical satellite. Coupled leaf-canopy-atmosphere Radiative Transfer Models (RTMs) allow linking vegetation variables directly to the at-sensor TOA radiance measured. Global Sensitivity Analysis (GSA) of RTMs enables the computation of the total contribution of each input variable to the output variance. We determined the impacts of the leaf-canopy-atmosphere variables into TOA radiance using the GSA to gain insights into retrievable variables. The leaf and canopy RTM PROSAIL was coupled with…

010504 meteorology & atmospheric sciencesradiative transfer models0211 other engineering and technologiesemulation02 engineering and technologytop-of-atmosphere radiance data01 natural sciencesEmulation; Global sensitivity analysis; Machine learning; MODTRAN; PROSAIL; Radiative transfer models; Retrieval; Sentinel-2; Top-of-atmosphere radiance dataKrigingRange (statistics)Radiative transferLeaf area indexlcsh:Scienceretrieval021101 geological & geomatics engineering0105 earth and related environmental sciencesRemote sensingMODTRANPROSAILMODTRANAtmospheric correctionradiative transfer models; global sensitivity analysis; emulation; machine learning; top-of-atmosphere radiance data; PROSAIL; MODTRAN; retrieval; Sentinel-2machine learningglobal sensitivity analysisLookup tableRadianceGeneral Earth and Planetary SciencesEnvironmental sciencelcsh:QSentinel-2Remote sensing
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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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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
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El Niño variability off Peru during the last 20,000 years

2005

Here we present a high-resolution marine sediment record from the El Nino region off the coast of Peru spanning the last 20,000 years. Sea surface temperature, photosynthetic pigments, and a lithic proxy for El Nino flood events on the continent are used as paleo–El Nino–Southern Oscillation proxy data. The onset of stronger El Nino activity in Peru started around 17,000 calibrated years before the present, which is later than modeling experiments show but contemporaneous with the Heinrich event 1. Maximum El Nino activity occurred during the early and late Holocene, especially during the second and third millennium B.P. The recurrence period of very strong El Nino events is 60–80 years. El…

010506 paleontology010504 meteorology & atmospheric sciencesFlood mythNorthern HemispherePaleontologyOceanography01 natural sciencesSea surface temperatureOceanographyEl Niño Southern OscillationEl Niño13. Climate actionClimatology14. Life underwaterYounger DryasHoloceneGeology0105 earth and related environmental sciencesPaleoceanography
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Large-scale, millennial-length temperature reconstructions from tree-rings

2018

Supported by the German Science Foundation, grants # Inst 247/665-1 FUGG and ES 161/9-1. SSG acknowledges support by the Alexander von Humboldt Foundation, KJA by US National Science Foundation grants AGS-1501856 and NSF AGS-1501834, and JL and LS by the Belmont Forum and JPI-Climate, Collaborative Research Action INTEGRATE. Over the past two decades, the dendroclimate community has produced various annually resolved, warm season temperature reconstructions for the extratropical Northern Hemisphere. Here we compare these tree-ring based reconstructions back to 831 CE and present a set of basic metrics to provide guidance for non-specialists on their interpretation and use. We specifically d…

010506 paleontology010504 meteorology & atmospheric sciencesNDASPlant ScienceWarm season01 natural sciencesG1Extratropical cycloneddc:550Little ice ageBeneficial effectsWarm season temperatures0105 earth and related environmental sciencesNorthern Hemisphereddc:333.7-333.9EcologyNorthern HemisphereG Geography (General)Medieval Warm PeriodCovarianceTree-ring widthMaximum latewood densityTree (data structure)ClimatologyLittle Ice AgeScale (map)Geology
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Concord and discord among Northern Hemisphere paleotemperature reconstructions from tree rings

2019

Abstract We review the current generation of large-scale, millennial-length temperature reconstructions derived from tree rings and highlight areas of agreement and disagreement among these state-of-the-art paleotemperature estimates. Although thousands of tree ring-width chronologies are now available from temperate and boreal forest sites across the Northern Hemisphere, only a small fraction of those records are suited as proxies for surface temperature. Maximum latewood density is clearly a superior temperature proxy but is less available, with few densitometric records that are both long and up-to-date. Compared to previous efforts, the newest generation of tree-ring reconstructions cor…

010506 paleontologyArcheologyGlobal and Planetary ChangeCurrent generationTemperature sensitivity010504 meteorology & atmospheric sciencesDivergence problemTaigaNorthern HemisphereGeologyDendroclimatology01 natural sciencesProxy (climate)ClimatologyTemperate climateEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesQuaternary Science Reviews
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Causes and consequences of past and projected Scandinavian summer temperatures, 500-2100 AD

2011

Tree rings dominate millennium-long temperature reconstructions and many records originate from Scandinavia, an area for which the relative roles of external forcing and internal variation on climatic changes are, however, not yet fully understood. Here we compile 1,179 series of maximum latewood density measurements from 25 conifer sites in northern Scandinavia, establish a suite of 36 subset chronologies, and analyse their climate signal. A new reconstruction for the 1483–2006 period correlates at 0.80 with June–August temperatures back to 1860. Summer cooling during the early 17th century and peak warming in the 1930s translate into a decadal amplitude of 2.9°C, which agrees with existin…

010506 paleontologyAtmospheric Science010504 meteorology & atmospheric sciencesAtmospheric circulationClimate ChangeClimate changelcsh:MedicineForcing (mathematics)Scandinavian and Nordic Countries01 natural sciencesAtmospheric CirculationBiospherePaleoclimatologyEnvironmental GeographyAtmospheric DynamicsPaleoclimatologylcsh:Science0105 earth and related environmental sciencesClimatologySeries (stratigraphy)MultidisciplinaryGeographyAtmospherelcsh:RTemperature/dk/atira/pure/core/subjects/geography15. Life on landSea surface temperatureGeographyPhysical Geography13. Climate actionClimate RecordClimatologyPeriod (geology)Earth SciencesClimate modellcsh:QSeasonsEnvironmental SciencesResearch ArticleClimate ModelingPLOS One
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Bioavailable 87Sr/86Sr in different environmental samples — Effects of anthropogenic contamination and implications for isoscapes in past migration s…

2012

(87)Sr/(86)Sr reference maps (isoscapes) are a key tool for investigating past human and animal migrations. However, there is little understanding of which biosphere samples are best proxies for local bioavailable Sr when dealing with movements of past populations. In this study, biological and geological samples (ground vegetation, tree leaves, rock leachates, water, soil extracts, as well as modern and archeological animal teeth and snail shells) were collected in the vicinity of two early medieval cemeteries ("Thuringians", 5-6th century AD) in central Germany, in order to characterize (87)Sr/(86)Sr of the local biosphere. Animal tooth enamel is not appropriate in this specific context t…

010506 paleontologyEnvironmental EngineeringFreshwater bivalveIsoscapesHuman MigrationSoil acidificationPopulationBiological AvailabilityContext (language use)Environmental pollution01 natural sciencesStrontium IsotopesAnimalsHumansEnvironmental Chemistry0601 history and archaeologyeducationWaste Management and Disposal0105 earth and related environmental scienceseducation.field_of_study060102 archaeologyEcologyBiosphereGeology06 humanities and the artsVegetation15. Life on landPollutionAnimal MigrationEnvironmental PollutionGeologyScience of The Total Environment
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Continental-scale temperature variability during the past two millennia

2013

Past global climate changes had strong regional expression. To elucidate their spatio-temporal pattern, we reconstructed past temperatures for seven continental-scale regions during the past one to two millennia. The most coherent feature in nearly all of the regional temperature reconstructions is a long-term cooling trend, which ended late in the nineteenth century. At multi-decadal to centennial scales, temperature variability shows distinctly different regional patterns, with more similarity within each hemisphere than between them. There were no globally synchronous multi-decadal warm or cold intervals that define a worldwide Medieval Warm Period or Little Ice Age, but all reconstructi…

010506 paleontologyPALAEOCLIMATE AND PALAEOCENOGRAPHYPaleoclimate010504 meteorology & atmospheric sciences[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]Climate change[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]910 Geography & travel01 natural sciencesCiencias de la Tierra y relacionadas con el Medio AmbienteInvestigación ClimatológicaCentennial550 Earth sciences & geology540 ChemistryPaleoclimatologyIce ageEarth temperaturePaleoclimatologySouthern Hemisphere0105 earth and related environmental sciencesCLIMATE SCIENCEAtmospherePaleoclimate; Temperature; Little Ice Age; Medieval Warm PeriodsTemperatureNorthern HemisphereClimatic changesScale (music)ClimatologyMedieval Warm PeriodsLittle Ice AgePeriod (geology)570 Life sciences; biologyGeneral Earth and Planetary SciencesCIENCIAS NATURALES Y EXACTASGeologyNature Geoscience
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Using growth and geochemical composition of Clathromorphum compactum to track multiscale North Atlantic hydro-climate variability

2020

International audience; Records of ocean/atmosphere dynamics over the past centuries are essential to understand processes driving climate variability. This is particularly true for the Northwest Atlantic which is a key region with an essential role in global climate regulation. Over the past two decades, coralline red algae have been increasingly used as environmental and climatic archives for the marine realm and hold the potential to extend long-term instrumental measurements. Here, we investigate the possibility to extract climate and environmental information from annual growth patterns and geochemical composition of the coralline red algae, Clathromorphum compactum, from Saint-Pierre …

010506 paleontologyPopulationClimate change010502 geochemistry & geophysicsOceanography01 natural sciencesCoralline algaeAtmosphereSclerochronologyEnvironmental reconstructionSclerochronologyClathromorphum compactumClimate change14. Life underwatereducationArctica islandicaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processeseducation.field_of_studygeographygeography.geographical_feature_categorybiologyACLEnvironmental proxyPaleontologyCoralline algaebiology.organism_classification13. Climate actionArchipelagoPhysical geography[SDE.BE]Environmental Sciences/Biodiversity and EcologyGeology
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