Widespread, Rapid Grounding Line Retreat of Pine Island, Thwaites, Smith, and Kohler Glaciers, West Antarctica, from 1992 to 2011. Rignot, E., Mouginot, J., Morlighem, M., Seroussi, H., & Scheuchl, B. 41(10):3502–3509.
Widespread, Rapid Grounding Line Retreat of Pine Island, Thwaites, Smith, and Kohler Glaciers, West Antarctica, from 1992 to 2011 [link]Paper  doi  abstract   bibtex   
We measure the grounding line retreat of glaciers draining the Amundsen Sea Embayment of West Antarctica using Earth Remote Sensing (ERS-1/2) satellite radar interferometry from 1992 to 2011. Pine Island Glacier retreated 31\,km at its center, with most retreat in 2005-2009 when the glacier un-grounded from its ice plain. Thwaites Glacier retreated 14\,km along its fast-flow core and 1 to 9\,km along the sides. Haynes Glacier retreated 10\,km along its flanks. Smith/Kohler glaciers retreated the most, 35\,km along its ice plain, and its ice shelf pinning points are vanishing. These rapid retreats proceed along regions of retrograde bed elevation mapped at a high spatial resolution using a mass conservation technique (MC) that removes residual ambiguities from prior mappings. Upstream of the 2011 grounding line positions, we find no major bed obstacle that would prevent the glaciers from further retreat and draw down the entire basin.
@article{rignotWidespreadRapidGrounding2014,
  title = {Widespread, Rapid Grounding Line Retreat of {{Pine Island}}, {{Thwaites}}, {{Smith}}, and {{Kohler}} Glaciers, {{West Antarctica}}, from 1992 to 2011},
  author = {Rignot, E. and Mouginot, J. and Morlighem, M. and Seroussi, H. and Scheuchl, B.},
  date = {2014-05},
  journaltitle = {Geophys. Res. Lett.},
  volume = {41},
  pages = {3502--3509},
  issn = {0094-8276},
  doi = {10.1002/2014gl060140},
  url = {https://doi.org/10.1002/2014gl060140},
  abstract = {We measure the grounding line retreat of glaciers draining the Amundsen Sea Embayment of West Antarctica using Earth Remote Sensing (ERS-1/2) satellite radar interferometry from 1992 to 2011. Pine Island Glacier retreated 31\,km at its center, with most retreat in 2005-2009 when the glacier un-grounded from its ice plain. Thwaites Glacier retreated 14\,km along its fast-flow core and 1 to 9\,km along the sides. Haynes Glacier retreated 10\,km along its flanks. Smith/Kohler glaciers retreated the most, 35\,km along its ice plain, and its ice shelf pinning points are vanishing. These rapid retreats proceed along regions of retrograde bed elevation mapped at a high spatial resolution using a mass conservation technique (MC) that removes residual ambiguities from prior mappings. Upstream of the 2011 grounding line positions, we find no major bed obstacle that would prevent the glaciers from further retreat and draw down the entire basin.},
  keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-13166886,antarctic-region,antarctic-sea-ice,climate-change,glaciers,global-warming,melting-acceleration,radar,remote-sensing,west-antartica},
  number = {10}
}
Downloads: 0