Cui Xiangbin

TL;DR: Bedmap2 as discussed by the authors is a suite of gridded products describing surface elevation, ice-thickness and the seafloor and subglacial bed elevation of the Antarctic south of 60° S. In particular, the Bedmap2 ice thickness grid is made from 25 million measurements, over two orders of magnitude more than were used in Bedmap1.

TL;DR: Radar information about the base of the ice at Dome A is presented, revealing classic Alpine topography with pre-existing river valleys overdeepened by valley glaciers formed when the mean summer surface temperature was around 3 °C, likely to have developed during the initial phases of Antarctic glaciation.

TL;DR: Cui et al. as mentioned in this paper reviewed both the recent progress of Chinese radioglaciological science in Antarctica and future proposed work, and estimated the age of the deep ice core at Kunlun Station through numerical modeling.

TL;DR: In this paper, the authors reviewed the progress of ice radar in investigating and researching Antarctic ice sheet thickness and subglacial topography, internal reflecting horizons,subglacial lakes and water systems, Subglacial bedrock roughness and crystal orientation fabrics(COF).