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

Ice caves are, similar to mountain glaciers, threatened by the warming climate. To better understand the response of perennial ice in caves to a changing climate, we analysed the thermal characteristics of a sag-type ice cave in the Austrian Alps (Hundsalm ice cave), based on long-term temperature m...

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Published in:The Cryosphere
Main Authors: M. Wind, F. Obleitner, T. Racine, C. Spötl
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2022
Subjects:
geo
Online Access:https://doi.org/10.5194/tc-16-3163-2022
https://tc.copernicus.org/articles/16/3163/2022/tc-16-3163-2022.pdf
https://doaj.org/article/141671e8124246d585f66b93c3bc304c
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:141671e8124246d585f66b93c3bc304c 2023-05-15T18:32:16+02:00 Multi-annual temperature evolution and implications for cave ice development in a sag-type ice cave in the Austrian Alps M. Wind F. Obleitner T. Racine C. Spötl 2022-08-01 https://doi.org/10.5194/tc-16-3163-2022 https://tc.copernicus.org/articles/16/3163/2022/tc-16-3163-2022.pdf https://doaj.org/article/141671e8124246d585f66b93c3bc304c en eng Copernicus Publications doi:10.5194/tc-16-3163-2022 1994-0416 1994-0424 https://tc.copernicus.org/articles/16/3163/2022/tc-16-3163-2022.pdf https://doaj.org/article/141671e8124246d585f66b93c3bc304c undefined The Cryosphere, Vol 16, Pp 3163-3179 (2022) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2022 fttriple https://doi.org/10.5194/tc-16-3163-2022 2023-01-22T17:50:41Z Ice caves are, similar to mountain glaciers, threatened by the warming climate. To better understand the response of perennial ice in caves to a changing climate, we analysed the thermal characteristics of a sag-type ice cave in the Austrian Alps (Hundsalm ice cave), based on long-term temperature measurements for the period 2008–2021. Observations show a warming trend in all parts of the cave as well as a distinct seasonal pattern with two main regimes, i.e. an open (winter) and a closed (summer) period. During the closed period, a persistent stable stratification prevails that largely decouples the cave from the external atmosphere. The open period is characterised by unstable to neutral stratification, which is an effect of convection during episodes when cold air can penetrate into the cave. Criteria to detect corresponding periods are investigated. Vertical temperature profiles also provide hints on corresponding circulation patterns and the spatial temperature variability in the cave. The positive air temperature trend is reflected in a decrease in perennial cave ice, derived from stake measurements. Besides surface melting, we find compelling evidence of basal melting of ice. The observed ablation rates can be well reproduced by applying a modified degree-day model, which, however, is less feasible regarding mass balance. Overall, we conclude that Hundsalm ice cave is highly impacted by regional warming, which will lead to the disappearance of its perennial ice deposits within the next decades. Article in Journal/Newspaper The Cryosphere Unknown The Cryosphere 16 8 3163 3179
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle geo
envir
M. Wind
F. Obleitner
T. Racine
C. Spötl
Multi-annual temperature evolution and implications for cave ice development in a sag-type ice cave in the Austrian Alps
topic_facet geo
envir
description Ice caves are, similar to mountain glaciers, threatened by the warming climate. To better understand the response of perennial ice in caves to a changing climate, we analysed the thermal characteristics of a sag-type ice cave in the Austrian Alps (Hundsalm ice cave), based on long-term temperature measurements for the period 2008–2021. Observations show a warming trend in all parts of the cave as well as a distinct seasonal pattern with two main regimes, i.e. an open (winter) and a closed (summer) period. During the closed period, a persistent stable stratification prevails that largely decouples the cave from the external atmosphere. The open period is characterised by unstable to neutral stratification, which is an effect of convection during episodes when cold air can penetrate into the cave. Criteria to detect corresponding periods are investigated. Vertical temperature profiles also provide hints on corresponding circulation patterns and the spatial temperature variability in the cave. The positive air temperature trend is reflected in a decrease in perennial cave ice, derived from stake measurements. Besides surface melting, we find compelling evidence of basal melting of ice. The observed ablation rates can be well reproduced by applying a modified degree-day model, which, however, is less feasible regarding mass balance. Overall, we conclude that Hundsalm ice cave is highly impacted by regional warming, which will lead to the disappearance of its perennial ice deposits within the next decades.
format Article in Journal/Newspaper
author M. Wind
F. Obleitner
T. Racine
C. Spötl
author_facet M. Wind
F. Obleitner
T. Racine
C. Spötl
author_sort M. Wind
title Multi-annual temperature evolution and implications for cave ice development in a sag-type ice cave in the Austrian Alps
title_short Multi-annual temperature evolution and implications for cave ice development in a sag-type ice cave in the Austrian Alps
title_full Multi-annual temperature evolution and implications for cave ice development in a sag-type ice cave in the Austrian Alps
title_fullStr Multi-annual temperature evolution and implications for cave ice development in a sag-type ice cave in the Austrian Alps
title_full_unstemmed Multi-annual temperature evolution and implications for cave ice development in a sag-type ice cave in the Austrian Alps
title_sort multi-annual temperature evolution and implications for cave ice development in a sag-type ice cave in the austrian alps
publisher Copernicus Publications
publishDate 2022
url https://doi.org/10.5194/tc-16-3163-2022
https://tc.copernicus.org/articles/16/3163/2022/tc-16-3163-2022.pdf
https://doaj.org/article/141671e8124246d585f66b93c3bc304c
genre The Cryosphere
genre_facet The Cryosphere
op_source The Cryosphere, Vol 16, Pp 3163-3179 (2022)
op_relation doi:10.5194/tc-16-3163-2022
1994-0416
1994-0424
https://tc.copernicus.org/articles/16/3163/2022/tc-16-3163-2022.pdf
https://doaj.org/article/141671e8124246d585f66b93c3bc304c
op_rights undefined
op_doi https://doi.org/10.5194/tc-16-3163-2022
container_title The Cryosphere
container_volume 16
container_issue 8
container_start_page 3163
op_container_end_page 3179
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