Monitoring Temperate Glacier Displacement by Multi-Temporal TerraSAR-X Images and Continuous GPS Measurements

被引:62
|
作者
Fallourd, Renaud [1 ]
Harant, Olivier [2 ]
Trouve, Emmanuel [1 ]
Nicolas, Jean-Marie [3 ]
Gay, Michel [2 ]
Walpersdorf, Andrea [4 ]
Mugnier, Jean-Louis [4 ]
Serafini, Jonathan [5 ]
Rosu, Diana [1 ]
Bombrun, Lionel [2 ]
Vasile, Gabriel [2 ]
Cotte, Nathalie [4 ]
Vernier, Flavien [1 ]
Tupin, Florence [3 ]
Moreau, Luc [6 ]
Bolon, Philippe [1 ]
机构
[1] Univ Savoie, LISTIC, Annecy, France
[2] INPG, Grenoble Image sPeech Signal Automat GIPSA Lab, Grenoble, France
[3] Telecom ParisTech, LTCI, Paris, France
[4] Grenoble Univ Savoie Chambery, Univ Grenoble 1, ISTerre, Grenoble, France
[5] Univ French Polynesia, Geosci Pacifique Sud Lab GePaSud, Tahiti, France
[6] Univ Savoie, EDYTEM, Chambery, France
关键词
Corner reflector (CR); high resolution (HR); motion estimation; offset tracking; synthetic aperture radar (SAR); temperate glacier; SAR; REGISTRATION; MOTION;
D O I
10.1109/JSTARS.2010.2096200
中图分类号
TM [电工技术]; TN [电子技术、通信技术];
学科分类号
0808 ; 0809 ;
摘要
A new generation of space-borne SAR sensors were launched in 2006-2007 with ALOS, TerraSAR-X, COSMO-Sky-Med and RadarSat-2 satellites. The data available in different bands (L, C and X bands), with High Resolution (HR) or multi-polarization modes offer new possibilities to monitor glacier displacement and surface evolution by SAR remote sensing. In this paper, the first results obtained with TerraSAR-X HR SAR image time series acquired over the temperate glaciers of the Chamonix Mont-Blanc test site are presented. This area involves well-known temperate glaciers which have been monitored and instrumented i. e. stakes for annual displacement/ ablation, GPS for surface displacement and cavitometer for basal displacement, for more than 50 years. The potential of 11-day repeated X-band HR SAR data for Alpine glacier monitoring is investigated by a combined use of in situ measurements and multi-temporal images. Interpretations of HR images, analysis of interferometric pairs and performance assessments of target/texture tracking methods for glacier motion estimation are presented. The results obtained with four time series covering the Chamonix Mont-Blanc glaciers over one year show that the phase information is rarely preserved after 11 days on such glaciers, whereas the high resolution intensity information allows the main glacier features to be observed and displacement fields on the textured areas to be derived.
引用
收藏
页码:372 / 386
页数:15
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