Search results for "Ice shelf"

showing 7 items of 7 documents

Seasonal changes in glacial polynya activity inferred from Weddell Sea varves

2013

Abstract. The Weddell Sea and the associated Filchner–Rønne Ice Shelf constitute key regions for global bottom-water production today. However, little is known about bottom-water production under different climate and ice-sheet conditions. Therefore, we studied core PS1795, which consists primarily of fine-grained siliciclastic varves that were deposited on contourite ridges in the southeastern Weddell Sea during the Last Glacial Maximum (LGM). We conducted high-resolution X-ray fluorescence (XRF) analysis and grain-size measurements with the RADIUS tool (Seelos and Sirocko, 2005) using thin sections to characterize the two seasonal components of the varves at sub-mm resolution to distingui…

Katabatic wind010504 meteorology & atmospheric sciencesStratigraphylcsh:Environmental protection010502 geochemistry & geophysics01 natural sciencesIce shelflcsh:Environmental pollutionSea icelcsh:TD169-171.8Glacial periodlcsh:Environmental sciences0105 earth and related environmental scienceslcsh:GE1-350Global and Planetary Changegeographygeography.geographical_feature_categoryPaleontologyLast Glacial MaximumBrine rejectionOceanography13. Climate actionlcsh:TD172-193.5Thermohaline circulationIce sheetGeologyClimate of the Past
researchProduct

Observation of classically 'forbidden' electromagnetic wave propagation and implications for neutrino detection.

2018

Ongoing experimental efforts in Antarctica seek to detect ultra-high energy neutrinos by measurement of radio-frequency (RF) Askaryan radiation generated by the collision of a neutrino with an ice molecule. An array of RF antennas, deployed either in-ice or in-air, is used to infer the properties of the neutrino. To evaluate their experimental sensitivity, such experiments require a refractive index model for ray tracing radio-wave trajectories from a putative in-ice neutrino interaction point to the receiving antennas; this gives the degree of signal absorption or ray bending from source to receiver. The gradient in the density profile over the upper 200 meters of Antarctic ice, coupled wi…

010504 meteorology & atmospheric sciencesWave propagationAstrophysics::High Energy Astrophysical PhenomenaFOS: Physical sciences01 natural sciencesElectromagnetic radiationAtomicIce shelfParticle and Plasma Physics0103 physical sciencesddc:530NuclearInstrumentation and Methods for Astrophysics (astro-ph.IM)Physics::Atmospheric and Oceanic Physics0105 earth and related environmental sciencesPhysicsHigh Energy Astrophysical Phenomena (astro-ph.HE)geographygeography.geographical_feature_categoryultra high energy photons and neutrinos010308 nuclear & particles physicsMolecularAstronomy and AstrophysicsNuclear & Particles PhysicsComputational physicsRay tracing (physics)Radio propagationNeutrino detectorcosmic ray experimentsNeutrinoAstrophysics - Instrumentation and Methods for AstrophysicsAstrophysics - High Energy Astrophysical PhenomenaAstronomical and Space SciencesRadio wave
researchProduct

Mise en évidence d’une dynamique de fleuves de glace durant la glaciation ordovicienne par l’enregistrement géomorphologique

2007

On Contemporary Ice streams the most important factor controlling polar ice-sheet sheet stability and ice flowing occurs in ice streams. On Pleistocene Ice Sheet, Ice stream can be located using several geomorphologic criteria predict from known characteristic of contemporary ice streams, these criteria defining the conceptual Ice Stream land system model. But nowadays, during fossil glaciations, ice streams characterization is still poorly documented and only few studies illustrate fast ice velocity. In this work, we characterize geomorphological markers of ice stream activity in order to define the Ordovician ice stream glacial landsystem. The study area is located in Sahara from Niger to…

Ice-sheet modelgeographygeography.geographical_feature_categoryFast iceIce streamSea iceAntarctic sea iceIce sheetGeomorphologySeabed gouging by iceGeologyIce shelfWater Science and TechnologyLa Houille Blanche
researchProduct

Influence of pre-existing microstructure on mechanical properties of marine ice during compression experiments

2014

AbstractMarine ice is an important component of ice shelves in Antarctica. It accretes in substantial amounts at weak points and below ice shelves. It is likely to exhibit peculiar rheological properties, which are crucial to understanding its potential role in stabilizing ice-shelf flow. Due to its location and consolidation processes, marine ice can present a variety of textures which are likely to influence its rheological properties. We present a new dataset of unconfined uniaxial compression experiments on folded marine ice samples that have been cut at various angles to the folds. Texture and fabric analyses are described ‘before’ and ‘after’ the deformation experiment. It is shown th…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesConsolidation (soil)MineralogyPressure ridge010502 geochemistry & geophysics01 natural sciencesIce shelfPhysics::GeophysicsCreepSea ice growth processesRheologyPerpendicularGeotechnical engineeringAstrophysics::Earth and Planetary AstrophysicsAnisotropyPhysics::Atmospheric and Oceanic PhysicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesJournal of Glaciology
researchProduct

Iodine emissions from the sea ice of the Weddell Sea

2012

Iodine compounds were measured above, below and within the sea ice of the Weddell Sea during a cruise in 2009, to make progress in elucidating the mechanism of local enhancement and volatilisation of iodine. I<sub>2</sub> mixing ratios of up to 12.4 pptv were measured 10 m above the sea ice, and up to 31 pptv was observed above surface snow on the nearby Brunt Ice Shelf – large amounts. Atmospheric IO of up to 7 pptv was measured from the ship, and the average sum of HOI and ICl was 1.9 pptv. These measurements confirm the Weddell Sea as an iodine hotspot. Average atmospheric concentrations of CH<sub>3</sub>I, C<sub>2</sub>H<sub>5</sub>I, CH&l…

0106 biological sciencesAtmospheric Science010504 meteorology & atmospheric sciencesIodidechemistry.chemical_element010501 environmental sciencesIodine01 natural sciencesIce shelflcsh:Chemistrychemistry.chemical_compoundSea iceIodate0105 earth and related environmental scienceschemistry.chemical_classificationgeographygeography.geographical_feature_category010604 marine biology & hydrobiologyFirnSnowlcsh:QC1-999ChemistryOceanographylcsh:QD1-999chemistry13. Climate actionSeawaterlcsh:PhysicsAtmospheric Chemistry and Physics
researchProduct

Biodiversity change after climate-induced ice-shelf collapse in the Antarctic

2011

Julian Gutt ... et al. -- 10 pages, 5 figures, 1 table, supplementary data https://doi.org/10.1016/j.dsr2.2010.05.024

0106 biological sciencesKrill010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global Changes[SDV.BID]Life Sciences [q-bio]/BiodiversityOceanography01 natural sciencesIce shelf1st insightsBenthosBenthosAntarctic PeninsulaEuphausia superba [Antarctic krill]EcosystemenEcosystemMarine ecosystem14. Life underwatersouthern-oceanKrillbiogeography0105 earth and related environmental sciences[ SDV.BID ] Life Sciences [q-bio]/Biodiversitygeography[ SDE.BE ] Environmental Sciences/Biodiversity and Ecologydeep-seageography.geographical_feature_categorybiologyaggregationsEcology010604 marine biology & hydrobiologyPelagic zone15. Life on landbiology.organism_classificationApex predatorsIceberg[ SDE.MCG ] Environmental Sciences/Global ChangesOceanographywestern weddell sea13. Climate actionBenthic zonepeninsulaDeep-sea speciesspecies-diversityimpactPioneer speciesross sea[SDE.BE]Environmental Sciences/Biodiversity and EcologyGeology
researchProduct

Total mercury and methyl-mercury contents and accumulation in polar microbial mats.

2014

Although polar regions are considered isolated and pristine areas, the organisms that inhabit these zones are exposed to global pollution. Heavy metals, such as mercury, are global pollutants and can reach almost any location on Earth. Mercury may come from natural, volcanic or geological sources, or result from anthropogenic sources, in particular industrial or mining activities. In this study, we have investigated one of the most prominent biological non-marine communities in both polar regions, microbial mats, in terms of their Hg and methyl-mercury (MeHg) concentrations and accumulation capacities. The main hypotheses posed argued on the importance of different factors, and to test them…

PollutionEnvironmental Engineeringmedia_common.quotation_subjectchemistry.chemical_elementIce shelfEnvironmental ChemistryMicrobial matWaste Management and Disposalmedia_commonShetlandPollutantgeographygeography.geographical_feature_categoryArctic RegionsMercuryMethylmercury CompoundsPollutionMercury (element)OceanographyArcticchemistryVolcanoBiofilmsEnvironmental scienceWater MicrobiologyWater Pollutants ChemicalEnvironmental MonitoringThe Science of the total environment
researchProduct