Data Summary

Summer surface mass balance of Bowdoin Glacier, Greenland in 2017

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    Summary

  • Aluminium poles were installed in the ice in the lower part of Bowdoin Glacier to measure surface mass balance. Length from top of the poles to ice surface was measured. Measured length change of the poles converted in meters water equivalent.

    Dataset citation

  • Sugiyama, S., D. Sakakibara, N. Kanna, S. Fukumoto, 2017, Summer surface mass balance of Bowdoin Glacier, Greenland in 2017, 1.00, Arctic Data archive System (ADS), Japan, https://ads.nipr.ac.jp/dataset/A20171127-004

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    Spatial coverage

  • N:  77.71°   S:  77.68°   E:  -68.54°   W:  -68.61°  

    Temporal coverage

  • 2017-07-07   -   2017-07-16

    License

  •  CC BY 4.0

DATA CONTORIBUTOR & GROUP

  • Shin Sugiyama
    (Institute of Low Temperature Science, Hokkaido University)
  • Daiki Sakakibara
    (Arctic Research Center, Hokkaido University)
  • Naoya Kanna
    (Arctic Research Center, Hokkaido University)
  • Shungo Fukumoto
    (Institute of Low Temperature Science, Hokkaido University)

PARAMETERS

  • GLACIER MASS BALANCE/ICE SHEET MASS BALANCE

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