Abstract
A portion of the Greenland ice sheet margin near the Jakobshavn area is mapped using an automatic, hierarchical approach applied to ERS-1 Synthetic Aperture Radar (SAR). Image tone and texture variability between the bare ice facies near the ice sheet margin and recently deglaciated rocks are used to map the ice sheet margin. This process involves integration of an anisotropic diffusion algorithm, local dynamic thresholding method, and edge following scheme.
| Original language | English |
|---|---|
| Pages | 148-150 |
| Number of pages | 3 |
| Publication status | Published - 1996 Jan 1 |
| Event | Proceedings of the 1996 International Geoscience and Remote Sensing Symposium, IGARSS'96. Part 1 (of 4) - Lincoln, NE, USA Duration: 1996 May 28 → 1996 May 31 |
Other
| Other | Proceedings of the 1996 International Geoscience and Remote Sensing Symposium, IGARSS'96. Part 1 (of 4) |
|---|---|
| City | Lincoln, NE, USA |
| Period | 96/5/28 → 96/5/31 |
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All Science Journal Classification (ASJC) codes
- Software
- Geology
Cite this
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Ice sheet margin detection using ERS-1 synthetic aperture radar. / Sohn, Hong Gyoo; Jezek, Kenneth C.
1996. 148-150 Paper presented at Proceedings of the 1996 International Geoscience and Remote Sensing Symposium, IGARSS'96. Part 1 (of 4), Lincoln, NE, USA, .Research output: Contribution to conference › Paper
TY - CONF
T1 - Ice sheet margin detection using ERS-1 synthetic aperture radar
AU - Sohn, Hong Gyoo
AU - Jezek, Kenneth C.
PY - 1996/1/1
Y1 - 1996/1/1
N2 - A portion of the Greenland ice sheet margin near the Jakobshavn area is mapped using an automatic, hierarchical approach applied to ERS-1 Synthetic Aperture Radar (SAR). Image tone and texture variability between the bare ice facies near the ice sheet margin and recently deglaciated rocks are used to map the ice sheet margin. This process involves integration of an anisotropic diffusion algorithm, local dynamic thresholding method, and edge following scheme.
AB - A portion of the Greenland ice sheet margin near the Jakobshavn area is mapped using an automatic, hierarchical approach applied to ERS-1 Synthetic Aperture Radar (SAR). Image tone and texture variability between the bare ice facies near the ice sheet margin and recently deglaciated rocks are used to map the ice sheet margin. This process involves integration of an anisotropic diffusion algorithm, local dynamic thresholding method, and edge following scheme.
UR - http://www.scopus.com/inward/record.url?scp=0029712426&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0029712426&partnerID=8YFLogxK
M3 - Paper
SP - 148
EP - 150
ER -