4.4 Article

Observed and modelled ice temperature and velocity along the main flowline of East Rongbuk Glacier, Qomolangma (Mount Everest), Himalaya

期刊

JOURNAL OF GLACIOLOGY
卷 59, 期 215, 页码 438-448

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CAMBRIDGE UNIV PRESS
DOI: 10.3189/2013JoG12J202

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资金

  1. National Fundamental Research Project (973) of China [2007CB411503]
  2. National Science Foundation of China (NSFC)

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Knowledge of present-day ice temperature and velocity is important in order to determine how fast a glacier will respond to present and future climate change. We apply a two-dimensional higher-order thermomechanical flowband model to simulate present-day ice temperature and velocity along the main flowline of East Rongbuk Glacier, Qomolangma (Mount Everest), Himalaya. We use recent (2005-11) observational data to validate the numerical model. Modelled and observed ice surface velocities exhibit good agreement. Modelled ice temperatures agree well with observed values in two shallow boreholes that are similar to 18 m deep. The model suggests that the ablation zone of East Rongbuk Glacier, km 4 to km 10 from the glacier head, is underlain by temperate ice.

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