क्यूआर कोड

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...

पूर्ण विवरण

में बचाया:
मुख्य लेखकों: Giuseppe Parrella, Irena Hajnsek, Konstantinos P. Papathanassiou
स्वरूप: Artigo
भाषा:Inglês
प्रकाशित: MDPI AG 2021-11-01
श्रृंखला:Remote Sensing
विषय:
Synthetic Aperture Radar
polarimetry
differential propagation
firn anisotropy
Greenland
ऑनलाइन पहुंच:https://www.mdpi.com/2072-4292/13/21/4448
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