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  4. Stream temperature and discharge evolution in Switzerland over the last 50 years: annual and seasonal behaviour
 
research article

Stream temperature and discharge evolution in Switzerland over the last 50 years: annual and seasonal behaviour

Michel, Adrien  
•
Brauchli, Tristan  
•
Lehning, Michael  
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January 10, 2020
Hydrology and Earth System Sciences

Stream temperature and discharge are key hydro- logical variables for ecosystem and water resource management and are particularly sensitive to climate warming. Despite the wealth of meteorological and hydrological data, few studies have quantified observed stream temperature trends in the Alps. This study presents a detailed analysis of stream temperature and discharge in 52 catchments in Switzerland, a country covering a wide range of alpine and lowland hydrological regimes. The influence of discharge, precipitation, air temperature, and upstream lakes on stream temperatures and their temporal trends is analysed from multi-decadal to seasonal timescales. Stream temperature has significantly increased over the past 5 decades, with positive trends for all four seasons. The mean trends for the last 20 years are + 0.37 ± 0.11 ◦ C per decade for water temperature, resulting from the joint effects of trends in air temperature (+0.39 ± 0.14 ◦C per decade), discharge (−10.1 ± 4.6 % per decade), and precipitation (−9.3±3.4% per decade). For a longer time period (1979–2018), the trends are +0.33 ± 0.03 ◦ C per decade for water temperature, +0.46±0.03°C per decade for air temperature, −3.0 ± 0.5 % per decade for discharge, and −1.3 ± 0.5 % per decade for precipitation. Furthermore, we show that snow and glacier melt compensates for air temperature warming trends in a transient way in alpine streams. Lakes, on the contrary, have a strengthening effect on downstream water temperature trends at all elevations. Moreover, the identified stream temperature trends are shown to have critical impacts on ecological and economical temperature thresholds (the spread of fish diseases and the usage of water for industrial cooling), especially in lowland rivers, suggesting that these waterways are becoming more vulnerable to the increasing air temperature forcing. Resilient alpine rivers are expected to become more vulnerable to warming in the near future due to the expected reductions in snow- and glacier-melt inputs. A detailed mathematical framework along with the necessary source code are provided with this paper.

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Type
research article
DOI
10.5194/hess-24-115-2020
Author(s)
Michel, Adrien  
Brauchli, Tristan  
Lehning, Michael  
Schaefli, Bettina  
Huwald, Hendrik  
Date Issued

2020-01-10

Published in
Hydrology and Earth System Sciences
Volume

24

Issue

1

Start page

115

End page

142

Subjects

Water temperature

•

Discharge

•

Climate change

•

Switzerland

•

Hydrology

Note

This article is licensed under a Creative Commons Attribution 4.0 International License

URL

Supplementary

https://www.hydrol-earth-syst-sci.net/24/115/2020/hess-24-115-2020-supplement.pdf
Editorial or Peer reviewed

REVIEWED

Written at

EPFL

EPFL units
CRYOS  
FunderGrant Number

Swiss federal funding

15.0003.PJ/Q1020785

RelationURL/DOI

IsSupplementedBy

https://zenodo.org/record/3603064
Available on Infoscience
January 13, 2020
Use this identifier to reference this record
https://infoscience.epfl.ch/handle/20.500.14299/164575
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