Articles | Volume 16, issue 8
https://doi.org/10.5194/tc-16-3163-2022
https://doi.org/10.5194/tc-16-3163-2022
Research article
 | 
05 Aug 2022
Research article |  | 05 Aug 2022

Multi-annual temperature evolution and implications for cave ice development in a sag-type ice cave in the Austrian Alps

Maria Wind, Friedrich Obleitner, Tanguy Racine, and Christoph Spötl

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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 tc-2022-67', Anonymous Referee #1, 29 Apr 2022
    • AC1: 'Reply on RC1', Maria Wind, 20 Jun 2022
  • RC2: 'Comment on tc-2022-67', Aurel Perşoiu, 07 Jun 2022
    • AC2: 'Reply on RC2', Maria Wind, 20 Jun 2022

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) (22 Jun 2022) by Ben Marzeion
AR by Maria Wind on behalf of the Authors (09 Jul 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (19 Jul 2022) by Ben Marzeion
AR by Maria Wind on behalf of the Authors (19 Jul 2022)  Author's response   Manuscript 
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Short summary
We present a thorough analysis of the thermal conditions of a sag-type ice cave in the Austrian Alps using temperature measurements for the period 2008–2021. Apart from a long-term increasing temperature trend in all parts of the cave, we find strong interannual and spatial variations as well as a characteristic seasonal pattern. Increasing temperatures further led to a drastic decrease in cave ice. A first attempt to model ablation based on temperature shows promising results.