Changes in air temperature, but not in precipitation, determine long-term trends in water chemistry of high mountain lakes of the Alps with and without rock glacier influence.

Alpine lakes Climate change Climate warming High elevation lakes Natural acidification Rock glacier impact

Journal

The Science of the total environment
ISSN: 1879-1026
Titre abrégé: Sci Total Environ
Pays: Netherlands
ID NLM: 0330500

Informations de publication

Date de publication:
20 Dec 2023
Historique:
received: 26 06 2023
revised: 24 09 2023
accepted: 09 10 2023
medline: 15 10 2023
pubmed: 15 10 2023
entrez: 14 10 2023
Statut: ppublish

Résumé

Climate change has strongly affected lakes around the world, but the relative effects of warmer air temperatures and changing precipitation on the water chemistry of alpine systems are not well understood. Here we tested the effect of monthly and seasonal climate on the water chemistry of six high mountain lakes located in the Alps. From 1982 to 2020, water samples were collected annually from different depths during the autumn mixing. We observed a simultaneous increase in electrical conductivity, ionic content, and pH with air temperature. In lakes with rock glacier influence, the increase in conductivity, ionic content, and especially in sulfate was even more pronounced, but accompanied by a strong decrease in pH. These differences are attributed to the direct influence of acidic meltwater from active rock glaciers in catchments with acidic bedrock. We then analyzed changes in lake chemistry, taking into account seasonal trends in air temperature and precipitation, using redundancy analysis. Temperature increase significantly affected water chemistry in five of the six lakes, especially at times of ice breakup. Increasing warming explained 17% to 32% of the changes in electrical conductivity, alkalinity, pH, major ions, and nitrogen. In contrast, precipitation had little effect on the changes of those parameters. Nevertheless, late spring snowfall and high snowfall in early fall, which result in prolonged ice cover, had a dampening effect on the impact of climate warming on lake chemistry. Our results confirm that climate warming remains a major driver of chemical changes in alpine lakes, but provide new evidence that late spring temperatures are the most important triggers.

Identifiants

pubmed: 37838057
pii: S0048-9697(23)06377-5
doi: 10.1016/j.scitotenv.2023.167750
pii:
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

167750

Informations de copyright

Copyright © 2023 The Authors. Published by Elsevier B.V. All rights reserved.

Déclaration de conflit d'intérêts

Declaration of competing interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Auteurs

Stefanie Schreder (S)

Department of Ecology, Universität Innsbruck, Technikerstr. 25, 6020 Innsbruck, Austria.

Ruben Sommaruga (R)

Department of Ecology, Universität Innsbruck, Technikerstr. 25, 6020 Innsbruck, Austria.

Roland Psenner (R)

Department of Ecology, Universität Innsbruck, Technikerstr. 25, 6020 Innsbruck, Austria; Present address: eurac Research, Drususalle 1/Viale Druso 1, 39100 Bolzano/Bozen, Italy.

Barbara Chimani (B)

GeoSphere Austria, Hohe Warte 38, 1190 Wien, Austria.

Manfred Ganekind (M)

GeoSphere Austria, Hohe Warte 38, 1190 Wien, Austria.

Karin A Koinig (KA)

Department of Ecology, Universität Innsbruck, Technikerstr. 25, 6020 Innsbruck, Austria. Electronic address: karin.koinig@uibk.ac.at.

Classifications MeSH