This data set contains past flow lines of Thwaites Glacier. The flow lines were identified using layer patterns tracked between parallel radar layers, from a radar profile of the Thwaites Glacier catchment. The radar data was run and processed by the University of Texas Institute for Geophysics. The flow lines were identified using internal layer patterns detected with radar. The patterns in the internal layers of glaciers were created upstream, and over time moved downstream.
Data are available via FTP in ASCII text (.txt) format.
The following example shows how to cite the use of this data set in a publication. For more information, see our Use and Copyright Web page.
The following example shows how to cite the use of this data set in a publication. List the principal investigators, year of data set release, data set title, publisher: NSIDC, and digital media.
Conway, H., G. Catania, and T. J. Fudge. 2010. Ice Flow History of the Thwaites Glacier, West Antarctica. Boulder, Colorado, USA: National Snow and Ice Data Center. http://dx.doi.org/10.7265/N5RR1W6X.
| Category | Description |
|---|---|
| Data format | Data are in ASCII text (.txt) format |
| Spatial coverage and resolution |
Southernmost Latitude: 79.7°S Northernmost Latitude: 76°S Westernmost Longitude: 99.5°W Easternmost Longitude: 123°W |
| Temporal coverage and resolution | Radar data were collected during the 2004 to 2005 Antarctic field season (October through February). |
| File naming convention | paleo_flow_line_picks.txt |
| File size | The data set consists of one 13 KB file. |
| Parameter(s) | X and Y coordinates that define a glacier flow line. |
| Procedures for obtaining data | Data are available via FTP. |
Dr. Howard Conway
Department of Earth and Space Sciences
University of Washington
Johnson Hall Rm-070, Box 351310
4000 15th Avenue NE
Seattle, WA 98195
USA
Dr. Ginny Catania
University of Texas Institute of Geophysics
J.J. Pickle Research Campus, Bldg. 196
10100 Burnet Road (R2200)
Austin, TX 78758
USA
T. J. Fudge
Department of Earth and Space Sciences
University of Washington
Johnson Hall
4000 15th Avenue NE
Seattle, WA 98195
USA
NSIDC User Services
National Snow and Ice Data Center
CIRES, 449 UCB
University of Colorado
Boulder, CO 80309-0449 USA
phone: +1 303.492.6199
fax: +1 303.492.2468
form: Contact NSIDC User Services
e-mail: nsidc@nsidc.org
This research was supported by NSF OPP grant 0739372.
This data set consists of one data file in ASCII text (.txt) format.
Data are available on the FTP site
in the ftp://sidads.colorado.edu/pub/DATASETS/AGDC/conway_nsidc_0463/ directory. The data set consists of one file, paleo_flow_line_picks.txt, which contains flow line data derived from a radar sounding of Thwaites Glacier in West Antarctica.
The data file is 13 KB.
The data were derived using radar sounding data collected from Thwaites Glacier in West Antarctica.
Southernmost Latitude: 79.7°S
Northernmost Latitude: 76°S
Westernmost Longitude: 99.5°W
Easternmost Longitude: 123°W
The radar data that support this investigation were collected by the University of Texas Institute for Geophysics during the Antarctic field season (October through February) in 2004 to 2005.
The data set contains a table of coordinates that define flow lines derived from a radar sounding of Thwaites Glacier in West Antarctica.
Each row contains two pairs of x and y coordinates, which form one flow line. Coordinates are in polar stereographic with units of kilometers (km). The parallel of true scale is 71°S.
| x1 | y1 | x2 | y2 |
| -1.3438309e+003 | -5.8595677e+002 | -1.3461408e+003 | -5.7038227e+002 |
| -1.3388820e+003 | -5.8459680e+002 | -1.3409560e+003 | -5.6897531e+002 |
| -1.3364551e+003 | -5.8392782e+002 | -1.3391090e+003 | -5.6846833e+002 |
Data are available via FTP.
The total volume of the data set is 13 KB.
Data are accessible using spreadsheet software.
Researchers identified past glacial flow lines for Thwaites Glacier in Antarctica using internal layer patterns detected with radar. The patterns in the internal layers of glaciers were created upstream, and over time moved downstream. By looking at the pattern between radar lines, researchers can discern the direction and timescale of past flow. The technique is described in more detail in Ng and Conway, 2004.
Holt, J. W., D. D. Blankenship, D. L. Morse, D. A. Young, M. E. Peters, S. D. Kempf, T. G. Richter, D. G. Vaughan, and H. F.J. Corr. 2006. New Boundary Conditions for the West Antarctic Ice Sheet: Subglacial Topography of the Thwaites and Smith Glacier Catchments. Geophysical Research Letters, Vol. 33, L09502, doi: 10.1029/2005GL025561.
Ng, F. and H. Conway. 2004. Fast-Flow Signature in the Stagnated Kamb Ice Stream. Geological Society of America 32:6, p. 481-484, doi:10.1130/G20317.1.
Table 1 lists related documents that are available online:
| Document | Description | URL |
|---|---|---|
| Antarctic Glaciological Data Center Web site | Data Center Web site | http://nsidc.org/agdc/ |
The acronyms used in this document are listed in Table 2.
| Acronym | Description |
|---|---|
| FTP | File Transfer Protocol |
| NSIDC | National Snow and Ice Data Center |
| URL | Uniform Resource Locator |
28 April 2010
http://nsidc.org/data/docs/nsidc0463_conway/index.html