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The Cryosphere An interactive open-access journal of the European Geosciences Union
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TC | Volume 12, issue 5
The Cryosphere, 12, 1767–1778, 2018
https://doi.org/10.5194/tc-12-1767-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
The Cryosphere, 12, 1767–1778, 2018
https://doi.org/10.5194/tc-12-1767-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 25 May 2018

Research article | 25 May 2018

Seasonal variations of the backscattering coefficient measured by radar altimeters over the Antarctic Ice Sheet

Fifi Ibrahime Adodo et al.
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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Fifi Adodo on behalf of the Authors (15 Feb 2018)  Author's response    Manuscript
ED: Publish subject to technical corrections (26 Apr 2018) by Robert Arthern
Publications Copernicus
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Short summary
In Antarctica, the seasonal cycle of the backscatter behaves differently at high and low frequencies, peaking in winter and in summer, respectively. At the intermediate frequency, some areas behave analogously to low frequency in terms of the seasonal cycle, but other areas behave analogously to high frequency. This calls into question the empirical relationships often used to correct elevation changes from radar penetration into the snowpack using backscatter.
In Antarctica, the seasonal cycle of the backscatter behaves differently at high and low...
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