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N-J. Schlegel, E. Larour, H. Seroussi, M. Morlighem and J. E. Box Decadal-scale sensitivity of Northeast Greenland ice flow to errors in surface mass balance using ISSM Journal of Geophysical Research: Earth Surface 118

Version of Record online: 20 MAY 2013 | DOI: 10.1002/jgrf.20062

Key Points

  • The model smooths ice velocities, even in response to extreme errors in forcing.
  • Mass flux is sensitive to local errors, but is affected by errors 200 km away.
  • Ice flow simulation requires a surface forcing resolution of at least 40 km.

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