IEDA
Dataset Information
Geophysical measurements Beardmore Glacier, Antarctica
Data DOI:
10.15784/601121
Cite as
Conway, H. (2018) "Geophysical measurements Beardmore Glacier, Antarctica" U.S. Antarctic Program (USAP) Data Center. doi: 10.15784/601121.
AMD - DIF Record(s)
Abstract
This data set contains radar-detected measurements of surface topography, ice thickness and derived bed topography across Beardmore Glacier and its tributary Mill Glacier.
Creator(s):
Conway, Howard
Date Created:
2018-09-09
Repository:
USAP-DC (current)
Spatial Extent(s)
West: 165.656, East: 172.155, South: -85.823, North: -83.357
Temporal Extent(s)
Start: 2014-12-01 - End: 2016-01-14
Award(s)
Version:
1
References
  1. Aster, R.C. and J P Winberry (2017). Glacial seismology. Reports on Progress in Physics, 80. (doi:10.1088/1361-6633/aa8473)
  2. Conway, H. and others (In Review). Direct evidence for channelized meltwater flow originating from beneath Beardmore Glacier, Antarctica. J. Glaciology.
  3. Cooley, J., Winberry, P., Koutnik, M., & Conway, H. (n.d.). Tidal and spatial variability of flow speed and seismicity near the grounding zone of Beardmore Glacier, Antarctica. Annals of Glaciology, 1-8. (doi:10.1017/aog.2019.14)
  4. Koutnik, M. and others (In Review) Assimilating glaciological and geochronological data into ice-flow models to constrain the deglaciation of Beardmore Glacier, Transantarctic Mountains. J. Glaciology.
Supplemental Docs
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README_601121.txt
Data Files
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1.2 MB
Beardmore_Glacier_Bed_Picks.zip