Search results for "Tine"

showing 10 items of 6703 documents

Types de temps et risque d'inondation et d'érosion en Camargue : diagnostique et prévision au 21ème siècle (1993-2100)

2010

High sea surges and waves are the two mains hydro-meteorological phenomenon associated with coastal flooding and erosion in Camargue. For the period 1993-2002, high monthly frequencies of strong surges are usually associated with high frequency of strong waves. These two phenomenons mainly occur during weather type showing a deep low pressure system over the Bay of Biscay associated with high pressure over Central Europe. The monthly frequency of such weather regime indicates the probability of occurrence of high surges and waves along Camargue's coast. During the 21st century, the frequency of this specific weather regime could stay stationary for the A1b climate change scenario.

"weather regimes" "sea surges" " waves" "Camargue coast" "climate change"[SHS.GEO] Humanities and Social Sciences/Geographytype de temps" " surcotes" "vague" "risque" "Camargue" "changement climatique[SDE.MCG]Environmental Sciences/Global Changes[SHS.GEO]Humanities and Social Sciences/Geography[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces environment[ SHS.GEO ] Humanities and Social Sciences/Geography[ SDE.MCG ] Environmental Sciences/Global Changes[SDE.MCG] Environmental Sciences/Global Changes[SDU.STU.CL] Sciences of the Universe [physics]/Earth Sciences/Climatology[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environment[ SDU.STU.CL ] Sciences of the Universe [physics]/Earth Sciences/Climatology[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment"type de temps" " surcotes" "vague" "risque" "Camargue" "changement climatique"
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The influence of decision-making in tree ring-based climate reconstructions.

2021

Tree-ring chronologies underpin the majority of annually-resolved reconstructions of Common Era climate. However, they are derived using different datasets and techniques, the ramifications of which have hitherto been little explored. Here, we report the results of a double-blind experiment that yielded 15 Northern Hemisphere summer temperature reconstructions from a common network of regional tree-ring width datasets. Taken together as an ensemble, the Common Era reconstruction mean correlates with instrumental temperatures from 1794–2016 CE at 0.79 (p < 0.001), reveals summer cooling in the years following large volcanic eruptions, and exhibits strong warming since the 1980s. Differing in…

/141/704/106/694010506 paleontology010504 meteorology & atmospheric sciencesScienceGeneral Physics and AstronomyClimate changePalaeoclimate01 natural sciencesArticleGeneral Biochemistry Genetics and Molecular BiologyPaleoclimatologySDG 13 - Climate ActionDendrochronologyddc:550Climate change[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment0105 earth and related environmental sciencesResearch dataddc:333.7-333.913 Climate ActionClimate change; Palaeoclimate; Research dataGEMultidisciplinaryQNorthern HemisphereDASGeneral ChemistryResearch data/706/648/697Geography13. Climate actionClimatology/704/106/413GE Environmental Sciences
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Extensions and corona decompositions of low-dimensional intrinsic Lipschitz graphs in Heisenberg groups

2020

This note concerns low-dimensional intrinsic Lipschitz graphs, in the sense of Franchi, Serapioni, and Serra Cassano, in the Heisenberg group $\mathbb{H}^n$, $n\in \mathbb{N}$. For $1\leq k\leq n$, we show that every intrinsic $L$-Lipschitz graph over a subset of a $k$-dimensional horizontal subgroup $\mathbb{V}$ of $\mathbb{H}^n$ can be extended to an intrinsic $L'$-Lipschitz graph over the entire subgroup $\mathbb{V}$, where $L'$ depends only on $L$, $k$, and $n$. We further prove that $1$-dimensional intrinsic $1$-Lipschitz graphs in $\mathbb{H}^n$, $n\in \mathbb{N}$, admit corona decompositions by intrinsic Lipschitz graphs with smaller Lipschitz constants. This complements results that…

01 natural sciencesmatemaattinen analyysiCombinatoricsCorona (optical phenomenon)Mathematics - Metric Geometry0103 physical sciencesHeisenberg groupClassical Analysis and ODEs (math.CA)FOS: MathematicsMathematics::Metric Geometry0101 mathematicsCommutative propertyPhysicsApplied MathematicsHeisenberg groups010102 general mathematicsMetric Geometry (math.MG)Lipschitz continuityGraphcorona decompositionMathematics - Classical Analysis and ODEs35R03 26A16 28A75low-dimensional intrinsic Lipschitz graphs010307 mathematical physicsmittateoriaLipschitz extension
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Influence of Wind on Suspended Matter in the Water of the Albufera of Valencia (Spain)

2021

Wind is one of the factors that has a great influence on suspended matter in lakes, especially in shallow lagoons. In order to know how wind affects the water in Albufera of Valencia, a shallow coastal lagoon, the measured variables of turbidity and transparency have been correlated with the estimates by processing Sentinel-2 satellite images with the Sen2Cor processor. Data from four years of study show that most of them are light to gentle easterly breezes and moderate to fresh westerly breezes. The results obtained show significant correlations between the measured variables and those obtained from the satellite images for total suspended matter and water transparency and with the averag…

010504 meteorology & atmospheric sciences0208 environmental biotechnologyOcean Engineering02 engineering and technologyAtmospheric sciences01 natural sciencesWind speedlcsh:Oceanographylcsh:VM1-989Wind effectlcsh:GC1-1581TurbidityEcologia de les albuferesShallow lakeValencia0105 earth and related environmental sciencesWater Science and TechnologyCivil and Structural EngineeringtransparencyHydrologySuspended solidsbiologySedimentlcsh:Naval architecture. Shipbuilding. Marine engineeringbiology.organism_classificationTransparency (behavior)atmospheric_science020801 environmental engineeringTotal suspended matterwind effectshallow lakeEnvironmental scienceSatellitesuspended solidsSentinel-2Suspended matter
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The WISE 2000 and 2001 Field Experiments in Support of the SMOS Mission:Sea Surface L-Band Brightness Temperature Observations and Their Application …

2004

Camps, Adriano ... et al.-- 20 pages, 16 figures, 3 tables

010504 meteorology & atmospheric sciences0211 other engineering and technologiesWind02 engineering and technologySea stateAtmospheric sciences01 natural sciencesOceanographic techniquesWind waveSurface roughnessEmissivitySeawater14. Life underwaterElectrical and Electronic EngineeringRadiometry[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment021101 geological & geomatics engineering0105 earth and related environmental sciencesRemote sensingPhysics[SDU.OCEAN]Sciences of the Universe [physics]/Ocean AtmosphereRadiometerFoamsOcean wavesRemote sensingSea surface temperature13. Climate actionBrightness temperatureGeneral Earth and Planetary SciencesSMOS MissionSignificant wave height
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Non‐subduction origin for 3.2 Ga high‐pressure metamorphic rocks in the Barberton granitoid‐greenstone terrane, South Africa

2019

The occurrence of high-pressure (HP) garnet-bearing metamorphic rocks in the southern Barberton granitoid-greenstone terrane (BGGT), South Africa, has been proposed as a key indicator of the onset of modern plate tectonics at ca. 3.2 Ga. Here, we report new zircon/titanite U-Pb ages of garnet-bearing HP metamorphic rocks and associated granitoids in the BGGT that argue against such an interpretation. The results show that HP metamorphism occurred synchronously with granitoid magmatism in the Stolzburg domain, the supposed subducted plate, during two episodes at 3.4 and 3.2 Ga, and that these two episodes of magmatism occurred on both sides of the assumed suture zone, a feature that cannot e…

010504 meteorology & atmospheric sciencesArcheanContinental crustGeochemistryMetamorphismGeologyCrust010502 geochemistry & geophysics01 natural sciencesMagmatismSuture (geology)Geology0105 earth and related environmental sciencesZirconTerraneTerra Nova
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The effect of rheological approximations in 3-D numerical simulations of subduction and collision

2018

Abstract Subduction and collision zones evolve differently from one another due to different rheological properties, different amounts of regional isostatic compensation, and the different mechanisms by which forces are applied to the convergent plates. The rheology of mantle and lithosphere is known to have the largest influence on the dynamics of subduction and continental collision. However, previous 3-D geodynamic models of subduction/collision processes have used various rheological approximations, making their results difficult to compare, since there is no clear understanding on the extent of these approximations on the dynamics. Here, we test the effect of rheological approximations…

010504 meteorology & atmospheric sciencesContinental collisionSubductionMechanics010502 geochemistry & geophysics01 natural sciencesMantle (geology)Physics::GeophysicsCondensed Matter::Soft Condensed MatterGeophysicsRheologyLithosphereTransition zoneSlabConvergent boundaryGeology0105 earth and related environmental sciencesEarth-Surface ProcessesTectonophysics
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Multiple intrusive phases in the Leinster Batholith, Ireland: geochronology, isotope geochemistry and constraints on the deformation history

2017

The formation of granite batholiths, commonly by incremental assembly of small magma batches, and their correlation with tectonic events, on both local and regional scales, is crucial to understanding the evolution of the Earth9s continental crust. However, these correlations often rely on assumptions about the detailed relationship and timing of mapped units. Here we report how an integrated geochronological, structural and isotope geochemical study in only one key locality from the late Caledonian Leinster Batholith in SE Ireland provides the potential for unravelling essential questions on batholith petrogenesis. The Northern Unit of the Leinster Batholith intruded incrementally, as demo…

010504 meteorology & atmospheric sciencesContinental crustGeochemistryGeology15. Life on land010502 geochemistry & geophysics01 natural sciences13. Climate actionBatholithIsotope geochemistryMagmaGeochronologyGeology0105 earth and related environmental sciencesWall rockZirconPetrogenesisJournal of the Geological Society
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Early Neoproterozoic crustal growth and microcontinent formation of the north–central Central Asian Orogenic Belt: New geological, geochronological, …

2021

Abstract In this study, new geological, geochronological, geochemical, and Nd–Hf isotopic data are presented for the Melange Zone within the Zavkhan terrane, Mongolia, and the terrane structure, early Neoproterozoic continental crust growth, and microcontinent formation in the north–central part of the Central Asian Orogenic Belt (CAOB) are discussed. The Melange Zone separates high-grade complexes of the northwestern part of the Zavkhan terrane and unmetamorphosed Neoproterozoic Zavkhan Formation covered by Cryogenian–Cambrian shelf deposits of the southwestern part. Zone consist of a lower-grade association of basalts, basaltic andesites, rarely felsic volcanic rocks, trondhjemites of the…

010504 meteorology & atmospheric sciencesContinental crustGeochemistryMetamorphismGeology010502 geochemistry & geophysics01 natural sciencesSupercontinentContinental arcContinental marginRodiniaIsland arcGeology0105 earth and related environmental sciencesTerraneGondwana Research
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Zircon and muscovite ages, geochemistry, and Nd-Hf isotopes for the Aktyuz metamorphic terrane: Evidence for an Early Ordovician collisional belt in …

2011

International audience; The Aktyuz metamorphic terrane in the Kyrgyz northern Tianshan consists of granitoid gneisses and migmatites with subordinate paragneisses, greenschists, presumed meta-ophiolites, and garnet amphibolite dykes that contain HP eclogite relicts. The gneisses and migmatites were previously considered to be Archaean and Palaeoproterozoic in age on the basis of α-Pb and U-Pb multigrain zircon dating. Zircons from a post-tectonic granite were previously dated at 692 ± 15 Ma, constraining the time of main deformation and metamorphism in the Aktyuz terrane to the Precambrian. The chemical characteristics of most granitoid samples are consistent with melting of chemically evol…

010504 meteorology & atmospheric sciencesContinental crustGeochemistryMetamorphism[SDU.STU]Sciences of the Universe [physics]/Earth SciencesGeology010502 geochemistry & geophysics01 natural sciencesDioritePrecambrian[SDU.STU] Sciences of the Universe [physics]/Earth SciencesEclogiteProtolithGeology0105 earth and related environmental sciencesZirconTerrane
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