Articles | Volume 19, issue 4
https://doi.org/10.5194/tc-19-1513-2025
https://doi.org/10.5194/tc-19-1513-2025
Research article
 | 
04 Apr 2025
Research article |  | 04 Apr 2025

Long-term development of a perennial firn aquifer on the Lomonosovfonna ice cap, Svalbard

Tim van den Akker, Ward van Pelt, Rickard Petterson, and Veijo A. Pohjola

Download

Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-1345', Anonymous Referee #1, 08 Jul 2024
    • AC1: 'Reply on RC1', Tim van den Akker, 03 Oct 2024
  • RC2: 'Comment on egusphere-2024-1345', Anonymous Referee #2, 27 Jul 2024
    • AC2: 'Reply on RC2', Tim van den Akker, 03 Oct 2024

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) (09 Oct 2024) by Wesley Van Wychen
AR by Tim van den Akker on behalf of the Authors (18 Nov 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (19 Nov 2024) by Wesley Van Wychen
RR by Anonymous Referee #1 (04 Dec 2024)
RR by Anonymous Referee #2 (16 Jan 2025)
ED: Publish subject to technical corrections (27 Jan 2025) by Wesley Van Wychen
AR by Tim van den Akker on behalf of the Authors (11 Feb 2025)  Manuscript 
Download
Short summary
Liquid water can persist within old snow on glaciers and ice caps if it can percolate into the snow before it refreezes. Snow is a good insulator, and it is porous where the percolated water can be stored. If this happens, the water piles up and forms a groundwater-like system. Here, we show observations of such a groundwater-like system found in Svalbard. We demonstrate that it behaves like a groundwater system and use that to model the development of the water table from 1957 until the present day.
Share