EGU23-15661
https://doi.org/10.5194/egusphere-egu23-15661
EGU General Assembly 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Elevation bias due to penetration of spaceborne radar signal on Grosser Aletschgletscher, Switzerland

Jacqueline Bannwart1, Livia Piermattei2,3, Inés Dussaillant1, Lukas Krieger4, Dana Floricioiu4, Etienne Berthier5, Claudia Roeoesli1, Horst Machguth6, and Michael Zemp1
Jacqueline Bannwart et al.
  • 1University of Zurich, Zürich, Switzerland (jacqueline.bannwart@geo.uzh.ch)
  • 2Department of Geosciences, University of Oslo, Norway
  • 3Remote Sensing Group, Research Unit Land Change Science, Swiss Federal Institute for Forest, Snow and Landscape Research WSL
  • 4Remote Sensing Technology Institute, DLR, Oberpfaffenhofen, Germany
  • 5Laboratoire d’Etudes en Géophysique et Océanographie Spatiales, Centre National de la Recherche Scientifique (LEGOS – CNRS, UMR5566), Université de Toulouse, France
  • 6Department of Geoscience, University of Fribourg, Switzerland

Digital elevation models (DEMs) from the spaceborne interferometric radar mission TanDEM-X hold a large potential for glacier elevation change assessments and monitoring. However, a bias is potentially introduced through the penetration of the X-band signal into snow and firn that can be substantial. The magnitude of this bias has been analysed in some glaciarized regions of the world; still, the knowledge about X-band penetration of TanDEM-X in the European Alps is limited.

In this study, we investigated the unique situation of almost synchronous acquisition of TanDEM-X and Pléiades DEMs over the Grosser Aletschgletscher, complemented with in-situ observations (ground penetrating radar, snow cores, snow pits), all within a four-day period in late winter 2021. The comparison of the TanDEM-X and Pléiades DEM revealed an elevation bias due to radar penetration of up to 8 m above 3400 m. Further, the concurrent in-situ measurements reveal that the signal is not obstructed by the last summer horizon but reaches into perennial firn.

Our study improves our understanding about the magnitude of X-band penetration of TanDEM-X in the Alps and the underlying process with a relevance for glaciology, snow science, remote sensing and the wider geoscience community.

How to cite: Bannwart, J., Piermattei, L., Dussaillant, I., Krieger, L., Floricioiu, D., Berthier, E., Roeoesli, C., Machguth, H., and Zemp, M.: Elevation bias due to penetration of spaceborne radar signal on Grosser Aletschgletscher, Switzerland, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-15661, https://doi.org/10.5194/egusphere-egu23-15661, 2023.