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Over-winter persistence of supraglacial lakes on the Greenland Ice Sheet: results and insights from a new model

Supporting Files


Details

  • Journal Title:
    Journal of Glaciology
  • Personal Author:
  • NOAA Program & Office:
  • Description:
    We present a newly developed 1-D numerical energy-balance and phase transition supraglacial lake model: GlacierLake. GlacierLake incorporates snowfall, in situ snow and ice melt, incoming water from the surrounding catchment, ice lid formation, basal freeze-up and thermal stratification. Snow cover and temperature are varied to test lake development through winter and the maximum lid thickness is recorded. Average wintertime temperatures of −2 to and total snowfall of 0 to 3.45 m lead to a range of the maximum lid thickness from 1.2 to 2.8 m after days, with snow cover exerting the dominant control. An initial ice temperature of with simulated advection of cold ice from upstream results in 0.6 m of basal freeze-up. This suggests that lakes with water depths above 1.3 to 3.4 m (dependent on winter snowfall and temperature) upon lid formation will persist through winter. These buried lakes can provide a sizeable water store at the start of the melt season, expedite future lake formation and warm underlying ice even in winter.
  • Keywords:
  • Source:
    Journal of Glaciology, 66(257), 362-372
  • DOI:
  • Document Type:
  • Rights Information:
    CC BY
  • Compliance:
    Submitted
  • Main Document Checksum:
    urn:sha256:0f667e804e71ba1d6772629676da532a1090f96f92004a4de271c4948b764086
  • Download URL:
  • File Type:
    Filetype[PDF - 1.54 MB ]
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