Climate Change-Induced Changes in the Chemistry of a High-Altitude Mountain Lake in the Central Alps ...

Mountains are among the most sensitive ecosystems to climate change, and one of the most evident signs of climate-related effect is the continuous net loss of ice from the cryosphere. Several studies showed that meltwater from glaciated and perennially frozen areas can profoundly affect alpine aquat...

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Main Authors: Steingruber, Sandra M., Bernasconi, Stefano M., Valenti, Giorgio
Format: Text
Language:English
Published: ETH Zurich 2021
Subjects:
Ice
Online Access:https://dx.doi.org/10.3929/ethz-b-000438687
http://hdl.handle.net/20.500.11850/438687
id ftdatacite:10.3929/ethz-b-000438687
record_format openpolar
spelling ftdatacite:10.3929/ethz-b-000438687 2024-09-30T14:36:26+00:00 Climate Change-Induced Changes in the Chemistry of a High-Altitude Mountain Lake in the Central Alps ... Steingruber, Sandra M. Bernasconi, Stefano M. Valenti, Giorgio 2021 application/pdf https://dx.doi.org/10.3929/ethz-b-000438687 http://hdl.handle.net/20.500.11850/438687 en eng ETH Zurich info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Climate change Mountain lake Alps Permafrost Rock glacier Water chemistry Text Journal Article ScholarlyArticle article-journal 2021 ftdatacite https://doi.org/10.3929/ethz-b-000438687 2024-09-02T07:54:09Z Mountains are among the most sensitive ecosystems to climate change, and one of the most evident signs of climate-related effect is the continuous net loss of ice from the cryosphere. Several studies showed that meltwater from glaciated and perennially frozen areas can profoundly affect alpine aquatic ecosystems. Here, we present the impressive temporal increase in solutes in Lake Leit, a mountain lake in the Central Alps that is impacted by an active rock glacier. During the last 30 years, concentrations of sulfate and base cations increased by factors of 4 and 3, respectively. Atmospheric deposition, the only catchment external source, could be excluded as possible cause. The inlets have sulfate and base cations concentrations that were up to double the concentrations of the lake outlet confirming the presence of catchment internal sources. The highest concentrations were measured in the springs at the bottom of the rock glacier. Ground surface temperatures of the rock glacier indicated a high probability ... : Aquatic Geochemistry, 27 (2) ... Text Ice permafrost DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Climate change
Mountain lake
Alps
Permafrost
Rock glacier
Water chemistry
spellingShingle Climate change
Mountain lake
Alps
Permafrost
Rock glacier
Water chemistry
Steingruber, Sandra M.
Bernasconi, Stefano M.
Valenti, Giorgio
Climate Change-Induced Changes in the Chemistry of a High-Altitude Mountain Lake in the Central Alps ...
topic_facet Climate change
Mountain lake
Alps
Permafrost
Rock glacier
Water chemistry
description Mountains are among the most sensitive ecosystems to climate change, and one of the most evident signs of climate-related effect is the continuous net loss of ice from the cryosphere. Several studies showed that meltwater from glaciated and perennially frozen areas can profoundly affect alpine aquatic ecosystems. Here, we present the impressive temporal increase in solutes in Lake Leit, a mountain lake in the Central Alps that is impacted by an active rock glacier. During the last 30 years, concentrations of sulfate and base cations increased by factors of 4 and 3, respectively. Atmospheric deposition, the only catchment external source, could be excluded as possible cause. The inlets have sulfate and base cations concentrations that were up to double the concentrations of the lake outlet confirming the presence of catchment internal sources. The highest concentrations were measured in the springs at the bottom of the rock glacier. Ground surface temperatures of the rock glacier indicated a high probability ... : Aquatic Geochemistry, 27 (2) ...
format Text
author Steingruber, Sandra M.
Bernasconi, Stefano M.
Valenti, Giorgio
author_facet Steingruber, Sandra M.
Bernasconi, Stefano M.
Valenti, Giorgio
author_sort Steingruber, Sandra M.
title Climate Change-Induced Changes in the Chemistry of a High-Altitude Mountain Lake in the Central Alps ...
title_short Climate Change-Induced Changes in the Chemistry of a High-Altitude Mountain Lake in the Central Alps ...
title_full Climate Change-Induced Changes in the Chemistry of a High-Altitude Mountain Lake in the Central Alps ...
title_fullStr Climate Change-Induced Changes in the Chemistry of a High-Altitude Mountain Lake in the Central Alps ...
title_full_unstemmed Climate Change-Induced Changes in the Chemistry of a High-Altitude Mountain Lake in the Central Alps ...
title_sort climate change-induced changes in the chemistry of a high-altitude mountain lake in the central alps ...
publisher ETH Zurich
publishDate 2021
url https://dx.doi.org/10.3929/ethz-b-000438687
http://hdl.handle.net/20.500.11850/438687
genre Ice
permafrost
genre_facet Ice
permafrost
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.3929/ethz-b-000438687
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