Automated detection and analysis of surface calving  waves with a terrestrial radar interferometer  at the front of Eqip Sermia, Greenland

Wehrlé, Adrien; Lüthi, Martin P.; Walter, Andrea; Jouvet, Guillaume; Vieli, Andreas

doi:https://doi.org/10.5194/tc-15-5659-2021

Articles | Volume 15, issue 12

The Cryosphere, 15, 5659–5674, 2021

https://doi.org/10.5194/tc-15-5659-2021

© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

The Cryosphere, 15, 5659–5674, 2021

https://doi.org/10.5194/tc-15-5659-2021

© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 15, issue 12

Research article 13 Dec 2021

Research article | 13 Dec 2021

Automated detection and analysis of surface calving waves with a terrestrial radar interferometer at the front of Eqip Sermia, Greenland

Adrien Wehrlé et al.

Model code and software

TeRACWA A. Wehrlé https://doi.org/10.5281/zenodo.5770016

Video supplement

Animation of consecutive TRI intensity images at the front of Eqip Sermia, Greenland A. Wehrlé https://doi.org/10.5281/zenodo.5602842

Short summary

We developed a novel automated method for the detection and the quantification of ocean waves generated by glacier calving. This method was applied to data recorded with a terrestrial radar interferometer at Eqip Sermia, Greenland. Results show a high calving activity at the glacier front sector ending in deep water linked with more frequent meltwater plumes. This suggests that rising subglacial meltwater plumes strongly affect glacier calving in deep water, but weakly in shallow water.