@article{oai:nipr.repo.nii.ac.jp:00015597,
 author = {Ai, Songtao and Wang, Shansi and Li, Yuansheng and Moholdt, Geir and Zhou, Chunxia and Liu, Leibao and Yang, Yuande},
 journal = {Polar Science},
 month = {Mar},
 note = {Dalk Glacier, which has been monitored by CHINARE since 2007, is a calving outlet glacier near the Chinese Zhongshan Station in East Antarctica. Using in situ observational azimuthal data from 2007 to 2012, 67 high-precision spatial intersection points were calculated. Consequently, the ice-flow features of the tongue of Dalk Glacier were explored via ground measurements. The maximum observed ice-flow velocity (IV) was 192.72 m/a, at stake P9. The velocities then decreased with the distance from the central flow line on both sides of the glacier in a cross section. Further analysis showed the following: the velocities of each stake increased annually; the closer to the terminus, the faster the ice flowed; and the ascent ratio of the IVs was approximately 10.67 m/a2 in the main flow area. We also observed seasonal variations in the ice-flow velocities, including a speed-up in January 2009 preceding an ice-calving event. The elevation change measurements at the stakes showed fluctuations along the central flow line, which indicates ice-shelf grounding over a seamount that had not been previously identified.},
 pages = {13--23},
 title = {High-precision ice-flow velocities from ground observations on Dalk Glacier, Antarctica},
 volume = {19},
 year = {2019}
}