Retrieval of Firn Thickness by Means of Polarisation Phase Differences in L-Band SAR Data

The knowledge of glacier zones’ extent and their temporal variations is fundamental for the retrieval of surface mass balance of glaciers and ice sheets. In this context, a key parameter is the firn line (FL), the lower boundary of the percolation zone, whose location is an indicator of time-integra...

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Auteurs principaux: Giuseppe Parrella, Irena Hajnsek, Konstantinos P. Papathanassiou
Format: article
Langue:EN
Publié: MDPI AG 2021
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Accès en ligne:https://doaj.org/article/e1025195a88c4d41bc494c28ecfd1ecd
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