Penetration of interferometric radar signals in Antarctic snow
<p>Synthetic aperture radar interferometry (InSAR) is an efficient technique for mapping the surface elevation and its temporal change over glaciers and ice sheets. However, due to the penetration of the SAR signal into snow and ice, the apparent elevation in uncorrected InSAR digital elevatio...
Main Authors: | H. Rott, S. Scheiblauer, J. Wuite, L. Krieger, D. Floricioiu, P. Rizzoli, L. Libert, T. Nagler |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2021-09-01
|
Series: | The Cryosphere |
Online Access: | https://tc.copernicus.org/articles/15/4399/2021/tc-15-4399-2021.pdf |
Similar Items
-
Changing pattern of ice flow and mass balance for glaciers discharging into the Larsen A and B embayments, Antarctic Peninsula, 2011 to 2016
by: H. Rott, et al.
Published: (2018-04-01) -
The imbalance of glaciers after disintegration of Larsen-B ice shelf, Antarctic Peninsula
by: H. Rott, et al.
Published: (2011-03-01) -
Impact of marine processes on flow dynamics of northern Antarctic Peninsula outlet glaciers
by: Helmut Rott, et al.
Published: (2020-06-01) -
Nordic Snow Radar Experiment
by: J. Lemmetyinen, et al.
Published: (2016-09-01) -
Evolution of surface velocities and ice discharge of Larsen B outlet glaciers from 1995 to 2013
by: J. Wuite, et al.
Published: (2015-05-01)