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| Content Provider | IEEE Xplore Digital Library |
|---|---|
| Author | Dierking, W. Haack, H. |
| Copyright Year | 1998 |
| Description | Author affiliation: Center for Remote Sensing, Tech. Univ., Lyngby, Denmark (Dierking, W.) |
| Abstract | Studies of radar scattering signatures typical for lava surfaces are needed in order to interprete SAR images of volcanic terrain on the Earth and on other planets, and to establish a physical basis for the choice of optimal radar configurations for geological mapping. The authors focus on a study of polarimetric L-band radar signatures observed over different lava flows located in the Northern Volcanic Zone in Iceland. Intensity images with a high spatial resolution are well suited for geological interpretation, both in the discrimination of lava flows from the surrounding terrain and in the recognition of different morphologic types within a flow. The largest contrasts are observed at cross-polarization. The phase difference between the VV- and HH-channels may provide information about a vegetation cover on the lava. The radar signal scattered from the flows is dominated by surface scattering contributions with a comparatively large fraction of multiple scattering. Other scattering mechanisms can not be recognized. |
| Starting Page | 1339 |
| Ending Page | 1341 |
| File Size | 249367 |
| Page Count | 3 |
| File Format | |
| ISBN | 0780344030 |
| DOI | 10.1109/IGARSS.1998.691402 |
| Language | English |
| Publisher | Institute of Electrical and Electronics Engineers, Inc. (IEEE) |
| Publisher Date | 1998-07-06 |
| Publisher Place | USA |
| Access Restriction | Subscribed |
| Rights Holder | Institute of Electrical and Electronics Engineers, Inc. (IEEE) |
| Subject Keyword | L-band Radar scattering Surface morphology Radar imaging Radar polarimetry Geology Synthetic aperture radar Earth Planets Terrain mapping |
| Content Type | Text |
| Resource Type | Article |
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