Service Interruption
 |
|
Antarctic Ice Velocity Data
|
Upper Ice Stream E (Landsat)
* These image maps are large and may require some time to load.
Image Information
The above overview map is a subscene from the USGS 1-km AVHRR mosaic (Ferrigno et al., 1996). Velocity data were derived from the Landsat scenes listed below. To view image data select Velocity Map or Data Set Map, or use the links on the overview image.
(*Note: This data corresponds to Area 4 in Journal of Glaciology, 1996, Vol. 42, No. 142, p.461-473, Bindschadler and others)
|
Satellite |
Image ID # |
Path/Row |
Date Acquired |
|---|
| Landsat 5 |
5014117008701710 |
14/117 |
17 January 1987 |
| Landsat 5 |
5014117009203110 |
14/117 |
31 January 1992 |
|
Corner coordinates for upper Ice Stream E velocity reference image: |
|---|
| Number of Lines: 5965 |
| Number of Samples: 6651 |
| Upper Left |
-77.964S |
-138.864W |
| Upper Right |
-79.162S |
-133.046W |
| Lower Left |
-78.864S |
-144.633W |
| Lower Right |
-80.169S |
-138.970W |
Both image co-registraion and velocity vectors are derived using the IMCORR software developed by Scambos et al. 1992 (see Related Publications). Typical co-registration errors are a few pixels. Because this error is constant for any image pair, it is treated as a systematic error within that image pair. Each cross-correlation match has an additional random error, typically about 0.3-0.5 pixels (Landsat resolution is 28.5 meters per pixel). IMCORR measures velocity as displacement divided by time separation, therefore, velocity errors scale as the inverse of the time interval. However, as time separation between the image pair increases, changes in the ice surface (e.g. crevasses, orientations, dunes, shear strain) result in fewer successful correlations.
While error in speed and error in bearing are reported, a more realistic error estimate is the combination of a systematic error of 1.5 pixels (42.75 meters) divided by time separation and a random error of 0.5 pixels (14.25 meters) divided by time separation. The reported speed and bearing errors are derived from the strength of the IMCORR feature correlation for each vector, and are therefore more related to precision than accuracy.
Access the tabular velocity data for Upper Ice Stream E
Top of Page
