Articles | Volume 28, issue 21
https://doi.org/10.5194/hess-28-4861-2024
https://doi.org/10.5194/hess-28-4861-2024
Research article
 | 
08 Nov 2024
Research article |  | 08 Nov 2024

Snowmelt-mediated isotopic homogenization of shallow till soil

Filip Muhic, Pertti Ala-Aho, Matthias Sprenger, Björn Klöve, and Hannu Marttila

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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-2023-884', Anonymous Referee #1, 22 Jul 2023
    • AC1: 'Reply on RC1 and RC2', Filip Muhic, 12 Sep 2023
  • RC2: 'Comment on egusphere-2023-884', Anonymous Referee #2, 08 Aug 2023
    • AC2: 'Reply on RC2 and RC1', Filip Muhic, 12 Sep 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (further review by editor and referees) (28 Oct 2023) by Markus Weiler
AR by Filip Muhic on behalf of the Authors (01 Feb 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (28 Feb 2024) by Markus Weiler
RR by Anonymous Referee #2 (21 Mar 2024)
ED: Publish subject to revisions (further review by editor and referees) (20 Apr 2024) by Markus Weiler
AR by Filip Muhic on behalf of the Authors (01 Jun 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (28 Jun 2024) by Markus Weiler
RR by Masaki Hayashi (29 Jul 2024)
ED: Publish as is (30 Jul 2024) by Markus Weiler
AR by Filip Muhic on behalf of the Authors (09 Aug 2024)  Manuscript 

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Filip Muhic on behalf of the Authors (16 Oct 2024)   Author's adjustment   Manuscript
EA: Adjustments approved (05 Nov 2024) by Markus Weiler
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Short summary
The snowmelt event governs the hydrological cycle of sub-arctic areas. In this study, we conducted a tracer experiment on a forested hilltop in Lapland to identify how high-volume infiltration events modify the soil water storage. We found that a strong tracer signal remained in deeper soil layers after the experiment and over the winter, but it got fully displaced during the snowmelt. We propose a conceptual infiltration model that explains how the snowmelt homogenizes the soil water storage.