Some Photogrammetric and Geodetic Aspects of Measurement of Glacier Surface Movement as Function of Time
Abstract The ice movement on the Byrd Glacier, Antarctica, was measured as function of time, on the basis of aerial photography. The method of aero-levelling strip triangulation with a minimum of geodetic control was applied. The methods and procedures were verified over Laufen-Bauma test area.
| Published in: | Journal of Glaciology |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Cambridge University Press (CUP)
1964
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1017/s002214300002880x https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S002214300002880X |