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  • Age; AGE; Age, lower confidence level; Age, upper confidence level; Age, ²¹⁰Pbₓₛ/¹³⁷Cs Lead-Caesium; Age model; DEPTH, sediment/rock; FOX12-02R; SEDCO; Sediment corer  (1)
  • Bathymetry  (1)
  • File content; File format; File name; File size; Greenland; NE_Greenland; Uniform resource locator/link to file  (1)
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  • 1
    Publication Date: 2023-12-15
    Description: A chronology was developed using ²¹⁰Pb excess (²¹⁰Pbₓₛ; T1/2 =22.3 yr) and ¹³⁷Cs (T1/2=30 years). Sediment samples were freeze dried, powdered and measured for radioisotopes on a low-background, well- type germanium detector. Activities of ²¹⁰Pb, ²²⁶Ra, and ¹³⁷Cs were corrected for self-adsorption and decay since core collection. The constant flux-constant sedimentation (CF-CS) approach was applied.
    Keywords: Age; AGE; Age, lower confidence level; Age, upper confidence level; Age, ²¹⁰Pbₓₛ/¹³⁷Cs Lead-Caesium; Age model; DEPTH, sediment/rock; FOX12-02R; SEDCO; Sediment corer
    Type: Dataset
    Format: text/tab-separated-values, 153 data points
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  • 2
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    PANGAEA
    In:  Supplement to: Mouginot, Jeremie P; Bjørk, Anders Anker; Millan, Romain; Scheuchl, Bernd; Rignot, Eric (2018): Insights on the surge behavior of Storstrømmen and L. Bistrup Brae, Northeast Greenland, over the last century. Geophysical Research Letters, 45(20), 11,197-11,205, https://doi.org/10.1029/2018GL079052
    Publication Date: 2023-12-16
    Description: The datasets describe the ice speed, grounding line positions and ice fronts of Storstrømmen and L. Bistrup Bræ located in Northeast Greenland. This data set consists of GeoTIFF (.tif) for the speed maps and ESRI shapefiles (.shp, .shx, .dbf, .prj) for the grounding lines and ice fronts. Surface ice velocity derived from feature or speckle tracking using declassified CORONA images from August 1967 and March 1968, Landsat-1&2/MSS images between 1973 and 1976, orthorectified American HEXAGON spy image acquired in1978 and 1982, Landsat-4&5/TM image pairs between 1984 and 1991, ERS-1/2 in 1993. GeoTIFF speed data are provided on polar stereographic projection. The file naming convention is first acquisition date (date1) followed by the second acquisition date (date2) and velocity component along x or y axis. (vx or v). Example : 19931231-19940118_vy.tif where date1=19931231, date2=19940118 and vy is the displacement along the y-axis. Grounding Lines position using InSAR data from the European Earth Remote Sensing (ERS-1/2) radar satellite collected in 1992 (3-day repeat cycle), in 1996 (1-day apart) and Sentinel-1a/b in Nov. 2015 and Apr. 2017. To digitize the grounding lines, we pick the inward limit of detection of vertical motion, where the glacier becomes afloat with a precision of about 50 m, as in Rignot et al., 2011. Ice fronts position between 1907 and 2015 from historical maps, aerial and satellite imagery.
    Keywords: File content; File format; File name; File size; Greenland; NE_Greenland; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 130 data points
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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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