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《Journal of Glaciology and Geocryology》 2003-06
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An Observation on Surface Ablation on the Yangbark Glacier in the Muztag Ata, China

PU Jian-chen, YAO Tan-dong, DUAN Ke-qinu Gansu 730000, China)  
During July 4 to August 8 in 2001, an observation of glacier ablation was made on the area between 4 460 m to 4 600 m a.s.l on the terminus of the Yangbark Glacier on the west of the Muztag Ata. Based on the observation, the ablation features are discussed in this paper. There existed a short warmer period on the glacier, with the maximum ablation mainly in July 21~22 and the maximum daily net ablation of about 144.5 mm water equivalent (w.e.) and 59.5 mm w.e. at the altitude of 4 460 m and 4 600 m a.s.l., respectively. The total net ablation reached to about 640~1 260 mm w.e. and the mean daily ablation about 26~32.8 mm w.e. during this period. Therefore, the annual net ablation is estimated about 1 700~2 000 mm w.e. in this region, which was far more than that of the glaciers on the inner Tibetan Plateau. Meanwhile, the ablation generally decreases with altitude. The ablation gradient is about 0.40~0.55 mm·10 m~{-1} on the bare ice and 0.21~3.53 mm/10 m on the debris-covered ice. So, the mean daily net ablation at the 4 800 m a.s.l. can be calculated from the ablation gradient on the bare ice. The glacier ablation continuously increases as compared with the observation in 1960 and 1987, according to the background of global warming.
【Fund】: 科技部前期研究项目(2001CCB00300);; 国家自然科学基金重大研究计划(90202013 90102005);; 国家自然科学基金项目(40101006 40171020)资助
【CateGory Index】: P343.6
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