Articles | Volume 17, issue 11
Research article
20 Nov 2023
Research article |  | 20 Nov 2023

Englacial architecture of Lambert Glacier, East Antarctica

Rebecca J. Sanderson, Kate Winter, S. Louise Callard, Felipe Napoleoni, Neil Ross, Tom A. Jordan, and Robert G. Bingham


Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on tc-2023-13', Steven Franke, 10 Mar 2023
    • AC1: 'Reply on RC1', Rebecca Sanderson, 26 May 2023
  • RC2: 'Comment on tc-2023-13', Marie G. P. Cavitte, 27 Mar 2023
    • AC2: 'Reply on RC2', Rebecca Sanderson, 26 May 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to revisions (further review by editor and referees) (04 Jul 2023) by Elisa Mantelli
AR by Rebecca Sanderson on behalf of the Authors (27 Jul 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (09 Aug 2023) by Elisa Mantelli
RR by Steven Franke (13 Aug 2023)
RR by Marie G. P. Cavitte (28 Aug 2023)
ED: Publish subject to technical corrections (07 Oct 2023) by Elisa Mantelli
AR by Rebecca Sanderson on behalf of the Authors (09 Oct 2023)  Manuscript 
Short summary
Ice-penetrating radar allows us to explore the internal structure of glaciers and ice sheets to constrain past and present ice-flow conditions. In this paper, we examine englacial layers within the Lambert Glacier in East Antarctica using a quantitative layer tracing tool. Analysis reveals that the ice flow here has been relatively stable, but evidence for former fast flow along a tributary suggests that changes have occurred in the past and could change again in the future.