Bed topography of Princess Elizabeth Land in East Antarctica

被引:46
|
作者
Cui, Xiangbin [1 ]
Jeofry, Hafeez [2 ,3 ]
Greenbaum, Jamin S. [4 ,5 ]
Guo, Jingxue [1 ]
Li, Lin [1 ]
Lindzey, Laura E. [6 ]
Habbal, Feras A. [7 ]
Wei, Wei [4 ]
Young, Duncan A. [4 ]
Ross, Neil [8 ]
Morlighem, Mathieu [9 ]
Jong, Lenneke M. [10 ,11 ]
Roberts, Jason L. [10 ,11 ]
Blankenship, Donald D. [4 ]
Bo, Sun [1 ]
Siegert, Martin J. [12 ,13 ]
机构
[1] Polar Res Inst China, Jinqiao Rd, Shanghai, Peoples R China
[2] Univ Malaysia Terengganu, Fac Sci & Marine Environm, Kuala Nerus, Terengganu, Malaysia
[3] Univ Malaysia Terengganu, Inst Oceanog & Environm, Kuala Nerus, Terengganu, Malaysia
[4] Univ Texas Austin, Inst Geophys, Jackson Sch Geosci, Austin, TX USA
[5] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA
[6] Univ Washington, Appl Phys Lab, Dept Ocean Engn, Seattle, WA 98105 USA
[7] Univ Texas Austin, Oden Inst Computat Engn & Sci, Austin, TX 78712 USA
[8] Newcastle Univ, Sch Geog Polit & Sociol, Newcastle Upon Tyne, Tyne & Wear, England
[9] Univ Calif Irvine, Dept Earth Syst Sci, Irvine, CA USA
[10] Australian Antarctic Div, Kingston, Tas, Australia
[11] Univ Tasmania, Inst Marine & Antarctic Studies, Hobart, Tas, Australia
[12] Imperial Coll London, Grantham Inst, London, England
[13] Imperial Coll London, Dept Earth Sci & Engn, London, England
基金
美国国家科学基金会; 国家重点研发计划; 中国国家自然科学基金;
关键词
ICE-SHEET; ELEVATION MODEL; WEST ANTARCTICA; GLACIER; THICKNESS; SYSTEM; RADAR; FLOW;
D O I
10.5194/essd-12-2765-2020
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
We present a topographic digital elevation model (DEM) for Princess Elizabeth Land (PEL), East Antarctica. The DEM covers an area of similar to 900000 km(2) and was built from radio-echo sounding data collected during four campaigns since 2015. Previously, to generate the Bedmap2 topographic product, PEL's bed was characterized from low-resolution satellite gravity data across an otherwise large (> 200 km wide) data-free zone. We use the mass conservation (MC) method to produce an ice thickness grid across faster flowing (> 30 m yr(-1)) regions of the ice sheet and streamline diffusion in slower flowing areas. The resulting ice thickness model is integrated with an ice surface model to build the bed DEM. Together with BedMachine Antarctica and Bedmap2, this new bed DEM completes the first-order measurement of subglacial continental Antarctica - an international mission that began around 70 years ago. The ice thickness data and bed DEMs of PEL (resolved horizontally at 500m relative to ice surface elevations obtained from the Reference Elevation Model of Antarctica - REMA) are accessible from https://doi.org/10.5281/zenodo.4023343 (Cui et al., 2020a) and https://doi.org/10.5281/zenodo.4023393 (Cui et al., 2020b).
引用
收藏
页码:2765 / 2774
页数:10
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