作者: Zhen Wu , Shiyin Liu , Shiqiang Zhang , Donghui Shangguan
DOI: 10.1007/S12583-013-0382-6
关键词: Glacier terminus 、 Glacial period 、 Geology 、 Thinning 、 Glacier mass balance 、 Geomorphology 、 Glacier 、 Ground-penetrating radar 、 Shuttle Radar Topography Mission 、 Digital elevation model 、 General 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.