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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Principais autores:	Giuseppe Parrella, Irena Hajnsek, Konstantinos P. Papathanassiou
格式:	Artigo
語言:	Inglês
出版:	MDPI AG 2021-11-01
叢編:	Remote Sensing
主題:	Synthetic Aperture Radar polarimetry differential propagation firn anisotropy Greenland
在線閱讀:	https://www.mdpi.com/2072-4292/13/21/4448
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