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

  • Renaud Fallourd
  • , Emmanuel Trouvé
  • , Diana Roşu
  • , Flavien Vernier
  • , Philippe Bolon
  • , Olivier Harant
  • , Michel Gay
  • , Lionel Bombrun
  • , Gabriel Vasile
  • , Jean Marie Nicolas
  • , Florence Tupin
  • , Andrea Walpersdorf
  • , Nathalie Cotte
  • , Jean Louis Mugnier
  • , Jonathan Serafini
  • , Luc Moreau
  • Universite de Savoie
  • Institut National Polytechnique de Grenoble (INPG)
  • CNRS LTCI
  • Université Joseph Fourier - Grenoble
  • University of French Polynesia
  • Université Savoie Mont Blanc

Résultats de recherche: Contribution à un journalArticleRevue par des pairs

Résumé

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.

langue originaleAnglais
Pages (de - à)372-386
Nombre de pages15
journalIEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing
Volume4
Numéro de publication2
Les DOIs
étatPublié - 1 janv. 2011
Modification externeOui

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