Accelerated thinning of Hei Valley No. 8 Glacier in the Tianshan Mountains, China

作者: Zhen Wu , Shiyin Liu , Shiqiang Zhang , Donghui Shangguan

DOI: 10.1007/S12583-013-0382-6

关键词: Glacier terminusGlacial periodGeologyThinningGlacier mass balanceGeomorphologyGlacierGround-penetrating radarShuttle Radar Topography MissionDigital elevation modelGeneral Earth and Planetary Sciences

摘要: Two field surveys on the thickness of Hei Valley No. 8 Glacier (H8) southern slope Mount Bogda in Tianshan (天山) Mountains using ground-penetration radar (GPR) were carried out August 2008 and September 2009. Comparisons observed change glacier GPR ablation stakes suggest that observations have high accuracy. Thus, for H8 during 2008–2009 was estimated data. Digital elevation models obtained from topographic maps Shuttle Radar Topography Mission used to analyze ice-elevation changes between 1 969 2 000 m a.s.l.. The results show has continually thinned, thinning rate increased gradually. areas 0.42±0.56 m/a 1969–2000 1.47±0.79 2000–2008, then accelerated 1.92±0.98 2008–2009. retreat terminus had a similar pattern. distribution temperate-ice zone as determined data also implies experienced strong melting 2009, which indicates temperature rises not only enhanced glacial surface prolonged periods, but changed englacial structure water content glacier, both probably lead acceleration thinning.

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