Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.


Science 28 November 1986:
Vol. 234. no. 4780, pp. 1105 - 1108
DOI: 10.1126/science.234.4780.1105

Articles

Antarctica: Measuring Glacier Velocity from Satellite Images

B. K. LUCCHITTA 1 and H. M. FERGUSON 1

1 U.S. Geological Survey, Flagstaff, AZ 86001.

Many Landsat images of Antarctica show distinctive flow and crevasse features in the floating part of ice streams and outlet glaciers immediately below their grounding zones. Some of the features, which move with the glacier or ice stream, remain visible over many years and thus allow time-lapse measurements of ice velocities. Measurements taken from Landsat images of features on Byrd Glacier agree well with detailed ground and aerial observations. The satellite-image technique thus offers a rapid and cost-effective method of obtaining average velocities, to a first order of accuracy, of many ice streams and outlet glaciers near their termini.

Submitted on June 16, 1986
Accepted on August 19, 1986


THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
Satellite-Image-Derived Velocity Field of an Antarctic Ice Stream.
R. A. Bindschadler, R. A. BINDSCHADLER, and T. A. SCAMBOS (1991)
Science 252, 242-246
   Abstract »    PDF »



To Advertise     Find Products


Science. ISSN 0036-8075 (print), 1095-9203 (online)