Articles | Volume 12, issue 5
https://doi.org/10.5194/tc-12-1767-2018
https://doi.org/10.5194/tc-12-1767-2018
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, Frédérique Remy, and Ghislain Picard

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

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
AR by Fifi Adodo on behalf of the Authors (03 May 2018)  Manuscript 
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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.