Search results for "glacier"

showing 10 items of 67 documents

Évolution contemporaine des glaciers arctiques: exemple de l'Austre Lovénbreen (79°N)

2016

International audience

changement climatiqueglacierArctique[SHS.GEO] Humanities and Social Sciences/Geography[SHS.GEO]Humanities and Social Sciences/GeographyComputingMilieux_MISCELLANEOUS[ SHS.GEO ] Humanities and Social Sciences/Geography
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Impact of Holocene climate variability on lacustrine records and human settlements in South Greenland

2015

Due to its sensitivity to climate changes, south Greenland is a particularly suitable area to study past global climate changes and their influence on locale Human settlements. A paleohydrological investigation was therefore carried out on two river-fed lakes: Lake Qallimiut and Little Kangerluluup, both located close to the Labrador Sea in the historic farming center of Greenland. Two sediment cores (QAL-2011 and LKG-2011), spanning the last four millennia, were retrieved and showed similar thin laminae, described by high magnetic susceptibility and density, high titanium and TOC / TN atomic ratio, and coarse grain size. They are also characterized either by inverse grading followed by nor…

geographygeography.geographical_feature_categoryFlood mythClimate changeSedimentGlacierOceanography13. Climate action[SDU]Sciences of the Universe [physics]Human settlement[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environmentPrecipitationIce sheet[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentGeologyHolocene[ SDU ] Sciences of the Universe [physics]
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Bacterial community structure along the subtidal sandy sediment belt of a high Arctic fjord (Kongsfjorden, Svalbard Islands)

2018

Open fjords are subject to contrasting environmental conditions, owing to meltwater glacial inputs, terrestrial runoff, and marine water mass exchanges, which are exacerbated by anthropogenic and climate perturbations. Following a slope-dependent water circulation, the subtidal sandy sediment belt regulates the convergent transport of nutrients downward the fjord depths, and the effective entrapment of suspended particles and microorganisms. In this study, we aimed at testing how glacial and seawater inputs may influence the bacterial community structure of subtidal sand deposits in the Kongsfjorden. Through total and viable cell counting and an amplicon sequencing approach, we found releva…

0301 basic medicineWater massEnvironmental EngineeringFjordmicrobial community compositioncoastal sands03 medical and health sciencesEnvironmental Chemistryta219Glacial periodMeltwaterglacial inputsWaste Management and Disposalgeographygeography.geographical_feature_categoryCommunityion PGM sequencingCommunity structureSedimentGlacierPollution030104 developmental biologyOceanographyCoastal sands Glacial inputs Ion PGM sequencing Microbial community composition Prokaryotic abundance Environmental Engineering Environmental Chemistry Waste Management and Disposal PollutionGeologyprokaryotic abundanceScience of the Total Environment
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Termini of calving glaciers as self-organized critical systems

2014

Calving margins are highly sensitive to changes in climate and glacier terminus geometry. Numerical modelling suggests that calving glacier termini are self-organized critical systems that are fluctuating between states of advance and retreat. Over the next century, one of the largest contributions to sea level rise will come from ice sheets and glaciers calving ice into the ocean1. Factors controlling the rapid and nonlinear variations in calving fluxes are poorly understood, and therefore difficult to include in prognostic climate-forced land-ice models. Here we analyse globally distributed calving data sets from Svalbard, Alaska (USA), Greenland and Antarctica in combination with simulat…

geographyGlacier terminusgeography.geographical_feature_categoryta114Tidewater glacier cycleIce calvingGlacierForcing (mathematics)Highly sensitiveSea level riseClimatologyGeneral Earth and Planetary SciencesIce sheetGeologyNature Geoscience
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Palaeogeographical relationships between Alpine and Jura glaciers during the two last Pleistocene glaciations

1992

Abstract Two main moraine complexes are usually defined in the northwestern Alpine piedmont: the External Moraine Complex (EMC) dated to the penultimate glaciation (“Riss” sensu lato) and the Internal Moraine Complex (IMC) dated to the last glaciation (“Wurm”). Until recently the prevalent concept was that these two complexes had been built by glaciers originating in the central Alpine zone. This paper presents a new palaeogeographical diagram, based on mapping and petrographical studies of these two moraine complexes, and especially on the relationships between Alpine and Jura tills. We reach the following conclusions. 1. (1) The Jura glaciers were independent of the Alpine glaciers during…

geographygeography.geographical_feature_categoryPleistocenePaleontologyAlpine climateGlacierOceanographyPaleontologyMoraineGlacial periodGeomorphologyEcology Evolution Behavior and SystematicsGeologyEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Subglacial bed deformation and dynamics of the Apriķi glacial tongue, W Latvia

2011

Saks, T., Kalvans, A. & Zelcs, V. 2012 (January): Subglacial bed deformation and dynamics of the Apriķi glacial tongue, W Latvia. Boreas, Vol. 41, pp. 124–140. 10.1111/j.1502-3885.2011.00222.x. ISSN 0300-9483. We evaluate the glacial dynamics and subglacial processes of the Apriķi glacial tongue in western Latvia during the Northern Lithuanian (Linkuva) oscillation of the last Scandinavian glaciation. The spatial arrangement of glacial bedforms and deformation structures are used to reconstruct the ice dynamics in the study area. The relationship between geological structures at the glacier bed and the spatial distribution of drumlins and glacigenic diapirs, on the one hand, and the permeab…

Archeologygeographygeography.geographical_feature_categoryBedformOldest DryasBedrockDrumlinGeologyGlacierDiapirFast iceGlacial periodGeomorphologyEcology Evolution Behavior and SystematicsGeologyBoreas
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Etude d'un système fluviatile proglaciaire par méthodes géophysiques et mesures GPS : L'exemple du glacier des Bossons

2007

[SDU.STU.AG] Sciences of the Universe [physics]/Earth Sciences/Applied geologyGPSGLACIERRADAR GEOLOGIQUE[ SDU.STU.AG ] Sciences of the Universe [physics]/Earth Sciences/Applied geology
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Heating glaciers from below

2013

Climate change is affecting the cryosphere from above. Geothermal heat flux from below is also contributing to conditions at the base of Greenland's ice sheet, which sits atop a lithosphere of variable thickness.

0303 health sciencesgeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeothermal heatingEarth scienceFluxClimate changeGlacierGeophysics01 natural sciences03 medical and health sciences13. Climate actionLithosphereGeneral Earth and Planetary SciencesCryosphereIce sheetSolid earthGeology030304 developmental biology0105 earth and related environmental sciencesNature Geoscience
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A discrete-element model for viscoelastic deformation and fracture of glacial ice

2015

a b s t r a c t A discrete-element model was developed to study the behavior of viscoelastic materials that are allowed to fracture. Applicable to many materials, the main objective of this analysis was to develop a model specifically for ice dynamics. A realistic model of glacial ice must include elasticity, brittle fracture and slow viscous deformations. Here the model is described in detail and tested with several benchmark simulations. The model was used to simulate various ice-specific applications with resulting flow rates that were compatible with Glen's law, and produced under fragmentation fragment-size distributions that agreed with the known analytical and experimental results.

Viscoelasticgeographygeography.geographical_feature_categoryta114IceDEMGeneral Physics and AstronomyGlacierMechanicsViscoelasticityPhysics::GeophysicsVolumetric flow rateIce dynamicsFragmentationHardware and ArchitectureDiscrete element modelElasticity (economics)Brittle fractureGeologyComputer Physics Communications
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Terrestrial Inputs Drive Seasonality in Organic Matter and Nutrient Biogeochemistry in a High Arctic Fjord System (Isfjorden, Svalbard)

2020

Climate-change driven increases in temperature and precipitation are leading to increased discharge of freshwater and terrestrial material to Arctic coastal ecosystems. These inputs bring sediments, nutrients and organic matter (OM) across the land-ocean interface with a range of implications for coastal ecosystems and biogeochemical cycling. To investigate responses to terrestrial inputs, physicochemical conditions were characterized in a river- and glacier-influenced Arctic fjord system (Isfjorden, Svalbard) from May to August in 2018 and 2019. Our observations revealed a pervasive freshwater footprint in the inner fjord arms, the geochemical properties of which varied spatially and seaso…

light climate0106 biological sciencesBiogeochemical cyclelcsh:QH1-199.5010504 meteorology & atmospheric sciencesFreshetOcean EngineeringFjordlcsh:General. Including nature conservation geographical distributionAquatic ScienceOceanographyPermafrost01 natural sciencesOrganic matterlcsh:Sciencecoastal biogeochemistryVDP::Landbruks- og Fiskerifag: 900::Fiskerifag: 920VDP::Mathematics and natural science: 4000105 earth and related environmental sciencesWater Science and Technologychemistry.chemical_classificationGlobal and Planetary Changegeographygeography.geographical_feature_category010604 marine biology & hydrobiologyAquatic ecosystemfreshwater inputsBiogeochemistryVDP::Matematikk og Naturvitenskap: 400dissolved organic matterglacier runoffclimate changeOceanographychemistryArcticEnvironmental sciencelcsh:Q
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