4.6 Article

Temperate ice layer found in the upper area of Jima Yangzong Glacier, the headstream of Yarlung Zangbo River

Journal

SCIENCE BULLETIN
Volume 61, Issue 8, Pages 619-621

Publisher

ELSEVIER
DOI: 10.1007/s11434-016-1045-7

Keywords

Jima Yangzong Glacier; Yarlung Zangbo River; Ground-penetrating radar; Radar velocity; Englacial water content; Polythermal

Funding

  1. Polar Atmospheric Science Field Base of CAMS [2016Z005]
  2. National Natural Science Foundation of China [41425003]
  3. National Fundamental Research Project (973) of China [2007CB411503]

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For the first time we investigate the basal thermal condition in the upper area of Jima Yangzong Glacier, the headstream of Yarlung Zangbo River, using ground-penetrating radar techniques. With common offset and common mid-point surveys we analyze the radar velocities in ice with respect to cold-temperate ice transition surface (0.1751 +/- 0.0028 m ns(-1)) and ice-bedrock interface (0.1657 +/- 0.0033 m ns(-1)), indicating a radar velocity of 0.1410 +/- 0.0154 m ns(-1) for the temperate ice layer (16.6 +/- 1.8 m). We estimate that the temperate ice layer has a water content of around 6 % +/- 4 %, suggesting that the Jima Yangzong Glacier, previously known as continental-type, now possibly becomes polythermal.

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