書誌事項
- 公開日
- 2010
- 権利情報
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- https://www.cambridge.org/core/terms
- DOI
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- 10.3189/002214311796406158
- 公開者
- International Glaciological Society
この論文をさがす
説明
<jats:title>Abstract</jats:title><jats:p>Spaceborne interferometric synthetic aperture radar (InSAR) techniques for measuring ice flow velocity and topography have developed rapidly over the last decade and a half, revolutionizing the study of ice dynamics. Spaceborne interferometry has contributed to major progress in many areas of glaciological study by: providing the first comprehensive measurements of ice-stream flow velocity over the major outlets of Greenland and Antarctica; revealing that ice-stream and outlet-glacier flow can change rapidly (months to years); improving understanding of several ice-sheet and ice-shelf processes; providing velocity for flux-gate based mass-balance assessment; mapping flow of mountain glaciers; and capturing the geomorphic traces of past ice flow. We review the basic technique development, the measurement characteristics, and the extensive set of results yielded by these measurements.</jats:p>
収録刊行物
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- Journal of Glaciology
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Journal of Glaciology 56 (200), 1026-1042, 2010
International Glaciological Society
