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  • Accumulation rate, standard deviation; Accumulation rate in ice equivalent per year; AGE; Antarctica; Distance; DomeC_area; Factor; Ground heat, flux; Ground heat, flux, standard deviation; Height; Ice thickness; LATITUDE; LONGITUDE; Melt rate; Melt rate, standard deviation; MULT; Multiple investigations; Number of years; Standard deviation  (1)
  • CALYPSO; Calypso Corer; Celtic Shelf; CH-NKS12; IMAGES; IMAGES I; International Marine Global Change Study; Marion Dufresne (1995); MD101; MD952002; MD95-2002; Meriadzec; NO-MKS03; PC; Piston corer  (1)
  • Mass conservation  (1)
Collection
Keywords
Years
  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Parrenin, Frédéric; Cavitte, Marie G P; Blankenship, Donald D; Chappellaz, Jérôme A; Fischer, Hubertus; Gagliardini, Olivier; Masson-Delmotte, Valerie; Passalacqua, Olivier; Ritz, Catherine; Roberts, Jason L; Siegert, Martin J; Young, Duncan A (2017): Is there 1.5-million-year-old ice near Dome C, Antarctica? The Cryosphere, 11(6), 2427-2437, https://doi.org/10.5194/tc-11-2427-2017
    Publication Date: 2023-03-31
    Description: Ice sheets provide exceptional archives of past changes in polar climate, regional environment and global atmospheric composition. The oldest dated deep ice core drilled in Antarctica has been retrieved at EPICA Dome C (EDC), reaching ~800,000 years. Obtaining an older paleoclimatic record from Antarctica is one of the greatest challenges of the ice core community. Here, we use internal isochrones, identified from airborne radar coupled to ice-flow modelling to estimate the age of basal ice along transects in the Dome C area. Three glaciological properties are inverted from isochrones: surface accumulation rate; geothermal flux; and the exponent of the Lliboutry velocity profile. We find that old ice (〉1 Myr, 1 million years) likely exists in two regions: one ~40 km south-west of Dome C along the ice divide to Vostok, close to a secondary dome that we name "Little Dome C" (LDC); and a second region named "North Patch" (NP) located 10-30 km north-east of Dome C, in a region where the geothermal flux is apparently relatively low. Our work demonstrates the value of combining radar observations with ice flow modelling to accurately represent the true nature of ice flow, and the formation of ice-sheet architecture, in the centre of large ice sheets.
    Keywords: Accumulation rate, standard deviation; Accumulation rate in ice equivalent per year; AGE; Antarctica; Distance; DomeC_area; Factor; Ground heat, flux; Ground heat, flux, standard deviation; Height; Ice thickness; LATITUDE; LONGITUDE; Melt rate; Melt rate, standard deviation; MULT; Multiple investigations; Number of years; Standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 95189 data points
    Location Call Number Expected Availability
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  • 2
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    Unknown
    PANGAEA
    In:  Supplement to: Auffret, Gérard A; Zaragosi, Sebastien; Dennielou, Bernard; Cortijo, Elsa; Van Rooij, David; Grousset, Francis E; Pujol, Claude; Eynaud, Frédérique; Siegert, Martin J (2002): Terrigenous fluxes at the Celtic Margin during the last glacial cycle. Marine Geology, 188(1-2), 79-108, https://doi.org/10.1016/S0025-3227(02)00276-1
    Publication Date: 2023-06-27
    Description: The sedimentary sections of three cores from the Celtic margin provide high-resolution records of the terrigenous fluxes during the last glacial cycle. A total of 21 14C AMS dates allow us to define age models with a resolution better than 100 yr during critical periods such as Heinrich events 1 and 2. Maximum sedimentary fluxes occurred at the Meriadzek Terrace site during the Last Glacial Maximum (LGM). Detailed X-ray imagery of core MD95-2002 from the Meriadzek Terrace shows no sedimentary structures suggestive of either deposition from high-density turbidity currents or significant erosion. Two paroxysmal terrigenous flux episodes have been identified. The first occurred after the deposition of Heinrich event 2 Canadian ice-rafted debris (IRD) and includes IRD from European sources. We suggest that the second represents an episode of deposition from turbid plumes, which precedes IRD deposition associated with Heinrich event 1. At the end of marine isotopic stage 2 (MIS 2) and the beginning of MIS 1 the highest fluxes are recorded on the Whittard Ridge where they correspond to deposition from turbidity current overflows. Canadian icebergs have rafted debris at the Celtic margin during Heinrich events 1, 2, 4 and 5. The high-resolution records of Heinrich events 1 and 2 show that in both cases the arrival of the Canadian icebergs was preceded by a European ice rafting precursor event, which took place about 1–1.5 kyr before. Two rafting episodes of European IRD also occurred immediately after Heinrich event 2 and just before Heinrich event 1. The terrigenous fluxes recorded in core MD95-2002 during the LGM are the highest reported at hemipelagic sites from the northwestern European margin. The magnitude of the Canadian IRD fluxes at Meriadzek Terrace is similar to those from oceanic sites.
    Keywords: CALYPSO; Calypso Corer; Celtic Shelf; CH-NKS12; IMAGES; IMAGES I; International Marine Global Change Study; Marion Dufresne (1995); MD101; MD952002; MD95-2002; Meriadzec; NO-MKS03; PC; Piston corer
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 3
    Publication Date: 2022-05-26
    Description: © The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Geophysical Research Letters 44 (2017): 11,051–11,061, doi:10.1002/2017GL074954.
    Description: Greenland's bed topography is a primary control on ice flow, grounding line migration, calving dynamics, and subglacial drainage. Moreover, fjord bathymetry regulates the penetration of warm Atlantic water (AW) that rapidly melts and undercuts Greenland's marine-terminating glaciers. Here we present a new compilation of Greenland bed topography that assimilates seafloor bathymetry and ice thickness data through a mass conservation approach. A new 150 m horizontal resolution bed topography/bathymetric map of Greenland is constructed with seamless transitions at the ice/ocean interface, yielding major improvements over previous data sets, particularly in the marine-terminating sectors of northwest and southeast Greenland. Our map reveals that the total sea level potential of the Greenland ice sheet is 7.42 ± 0.05 m, which is 7 cm greater than previous estimates. Furthermore, it explains recent calving front response of numerous outlet glaciers and reveals new pathways by which AW can access glaciers with marine-based basins, thereby highlighting sectors of Greenland that are most vulnerable to future oceanic forcing.
    Description: National Aeronautics and Space Administration; Cryospheric Sciences Program Grant Number: NNX15AD55G; National Science Foundation's ARCSS program Grant Number: 1504230; NERC Grant Number: NE/M000869/1
    Keywords: Greenland ; Bathymetry ; Mass conservation ; Multibeam echo sounding ; Radar echo sounding ; Glaciology
    Repository Name: Woods Hole Open Access Server
    Type: Article
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