Articles | Volume 18, issue 11
https://doi.org/10.5194/tc-18-5431-2024
https://doi.org/10.5194/tc-18-5431-2024
Research article
 | 
25 Nov 2024
Research article |  | 25 Nov 2024

Assessing supraglacial lake depth using ICESat-2, Sentinel-2, TanDEM-X, and in situ sonar measurements over Northeast and Southwest Greenland

Katrina Lutz, Lily Bever, Christian Sommer, Thorsten Seehaus, Angelika Humbert, Mirko Scheinert, and Matthias Braun

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-1244', Laura Melling, 17 Jun 2024
    • RC2: 'Quick edit to RC1', Laura Melling, 18 Jun 2024
      • AC1: 'Reply on RC1', Katrina Lutz, 25 Jul 2024
    • AC1: 'Reply on RC1', Katrina Lutz, 25 Jul 2024
  • RC3: 'Comment on egusphere-2024-1244', Devon Dunmire, 20 Jun 2024
    • AC3: 'Reply on RC3', Katrina Lutz, 26 Jul 2024
  • CC1: 'Comment on Lutz et al. (2024): "Assessing supraglacial lake depth using ICESat-2, Sentinel-2, TanDEM-X, and in situ sonar measurements over Northeast Greenland"', Philipp Arndt, 02 Jul 2024
    • AC2: 'Reply on CC1', Katrina Lutz, 25 Jul 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (01 Oct 2024) by Nicholas Barrand
AR by Katrina Lutz on behalf of the Authors (02 Oct 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (02 Oct 2024) by Nicholas Barrand
AR by Katrina Lutz on behalf of the Authors (02 Oct 2024)  Author's response   Manuscript 
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Short summary
The estimation of the amount of water found within supraglacial lakes is important for understanding how much water is lost from glaciers each year. Here, we develop two new methods for estimating supraglacial lake volume that can be easily applied on a large scale. Furthermore, we compare these methods to two previously developed methods in order to determine when it is best to use each method. Finally, three of these methods are applied to peak melt dates over an area in Northeast Greenland.