Historical surface mass balance from a frequency-modulated continuous-wave (FMCW) radar survey from Zhongshan station to Dome A

• Published in: Journal of Glaciology
• Main Authors: Jingxue Guo, Wangxiao Yang, Yinke Dou, Xueyuan Tang, Jamin S. Greenbaum, Ruofan Dou, Yao Pan, Yuzhong Zhang, Minghu Ding, Su Jiang, Guitao Shi, Xiangbin Cui, Bo Sun
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press 2020
• Subjects: Antarctic glaciology; climate change; ice core; ice-sheet mass balance; radio-echo sounding; Environmental sciences; GE1-350; Meteorology. Climatology; QC851-999; Antarctic; Zhongshan; Zhongshan Station; Antarc*; Antarctica; Ice Sheet; Journal of Glaciology
• Online Access: https://doi.org/10.1017/jog.2020.58; https://doaj.org/article/9705bef2807f4f76b2c840aa2e12ee73

Using frequency-modulated continuous wave radar data from the 32nd Chinese Antarctic Research Expedition in 2015/16, subsurface profiles were obtained along an East Antarctic inland traverse from Zhongshan station to Dome A, and four distinct regions were selected to analyze the spatiotemporal variability in historical surface mass balance (SMB). Based on depth, density, and age data from ice cores along the traverse, the radar data were calibrated to yield average SMB data. The zone 49–195 km from the coast has the highest SMB (235 kg m−2 a−1). The 780–892 km zone was most affected by the Medieval Warm Period and the Little Ice Age, and the SMB during ad 1454–1836 (71 kg m−2 a−1) was only one-quarter of that in the 20th century. The SMB in the 1080–1157 km zone fluctuates the most, possibly due to erosion or irregular deposition of snow by katabatic winds in low SMB areas with surface elevation fluctuations. Dome A (1157–1236 km) has the lowest SMB (29 kg m−2 a−1) and did not decrease during Little Ice Age. Understanding the spatiotemporal variability of SMB in a larger space can help us understand the complex climate history of Antarctica.