Articles | Volume 13, issue 10
https://doi.org/10.5194/tc-13-2579-2019
https://doi.org/10.5194/tc-13-2579-2019
Research article
 | 
02 Oct 2019
Research article |  | 02 Oct 2019

Spatial and temporal variations in basal melting at Nivlisen ice shelf, East Antarctica, derived from phase-sensitive radars

Katrin Lindbäck, Geir Moholdt, Keith W. Nicholls, Tore Hattermann, Bhanu Pratap, Meloth Thamban, and Kenichi Matsuoka

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (07 Aug 2019) by Nanna Bjørnholt Karlsson
AR by Katrin Lindbäck on behalf of the Authors (08 Aug 2019)  Author's response    Manuscript
ED: Publish subject to technical corrections (15 Aug 2019) by Nanna Bjørnholt Karlsson
Download
Short summary
In this study, we used a ground-penetrating radar technique to measure melting at high precision under Nivlisen, an ice shelf in central Dronning Maud Land, East Antarctica. We found that summer-warmed ocean surface waters can increase melting close to the ice shelf front. Our study shows the use of and need for measurements in the field to monitor Antarctica's coastal margins; these detailed variations in basal melting are not captured in satellite data but are vital to predict future changes.