通知: ·180511 张栋博士报告    ·180511 软件使用讲座    ·180511 祁诗阳博士报告    ·180504 SEN博士学术报告    ·180426 研究生交流会   




  2014年 (15)
  2013年 (8)
  2012年 (11)

发表论文 您的位置是: 首页 > 科学研究 > 研究成果 > 发表论文 > 正文


2018 High-Resolution Interannual Mass Anomalies of the Antarctic Ice Sheet by Combining GRACE Gravimetry and ENVISAT Altimetry

发布时间:2018-01-05          来源:           浏览次数:

Xiaoli Su, C. K. Shum, Junyi Guo, Ian M. Howat, Chungyen Kuo, Kenneth C. Jezek, Jianbin Duan, and Yuchan Yi


X. Su is with the MOE Key Laboratory of Fundamental Physical Quantities Measurement, Hubei Key Laboratory of Gravitation and Quantum Physics, Institute of Geophysics, School of Physics, Huazhong University of Science and Technology, Wuhan 430074, China (e-mail: xisu2016@hust.edu.cn).


Abstract—Knowledge of interannual mass variations of the Antarctic ice sheet (AIS) associated with its surface mass change is important for correctly interpreting the long-term mass trend and evaluating the fidelity of surface mass balance from regional climate models. Here, we revisit the interannual anomalies of mass change from Gravity Recovery and Climate Experiment and elevation change from ENVISAT over the AIS during 2003–2009, with the objective of obtaining higher resolution interannual mass anomalies based on ENVISAT data. High positive correlations (>0.6) between the two interannual anomalies are primarily found over the west AIS and coastal regions in the east AIS, occupying more than 40% of the AIS. By combining the two interannual anomalies, we are able to estimate the density of snow/ice changing interannually over regions in the AIS. Especially over the Amundsen Sea sector with significant interannual signals, the temporal variability of the density of snow/ice associated with interannual anomalies is shown for the first time, which agrees with the events of excess snow accumulation and the accelerated ice discharge occurring there. Furthermore, we demonstrate the feasibility of obtaining higher resolution interannual mass anomalies over the west AIS, based on the density-corrected ENVISAT data. Negative correlations, which were also found in a previous study, are likely related to errors in the relatively weak interannual signals.


DOI: 10.1109/TGRS.2017.2751070

上一篇:2018 Dependence of quality factor on surface roughness in crystalline whispering-gallery mode resonators
下一篇:2017 The gravity field model IGGT_R1 based on the second invariant of the GOCE gravitational gradient tensor

Copyright (C) 华中科技大学引力中心 地址:湖北省武汉市洪山区珞喻路1037号 邮编:430074