Increasing maximum lake surface temperature under climate change

[thumbnail of Open Access]
Preview
Text (Open Access) - Published Version
· Available under License Creative Commons Attribution.
· Please see our End User Agreement before downloading.
| Preview
Available under license: Creative Commons Attribution

Please see our End User Agreement.

It is advisable to refer to the publisher's version if you intend to cite from this work. See Guidance on citing.

Add to AnyAdd to TwitterAdd to FacebookAdd to LinkedinAdd to PinterestAdd to Email

Dokulil, M. T. orcid id iconORCID: https://orcid.org/0000-0002-6369-1457, de Eyto, E. orcid id iconORCID: https://orcid.org/0000-0003-2281-2491, Maberly, S. C. orcid id iconORCID: https://orcid.org/0000-0003-3541-5903, May, L. orcid id iconORCID: https://orcid.org/0000-0003-3385-9973, Weyhenmeyer, G. A. orcid id iconORCID: https://orcid.org/0000-0002-4013-2281 and Woolway, R. I. orcid id iconORCID: https://orcid.org/0000-0003-0498-7968 (2021) Increasing maximum lake surface temperature under climate change. Climatic Change, 165 (3-4). 56. ISSN 0165-0009 doi: 10.1007/s10584-021-03085-1

Abstract/Summary

Annual maximum lake surface temperature influences ecosystem structure and function and, in particular, the rates of metabolic activities, species survival and biogeography. Here, we evaluated 50 years of observational data, from 1966 to 2015, for ten European lakes to quantify changes in the annual maximum surface temperature and the duration above a potentially critical temperature of 20 °C. Our results show that annual maximum lake surface temperature has increased at an average rate of +0.58 °C decade−1 (95% confidence interval 0.18), which is similar to the observed increase in annual maximum air temperature of +0.42 °C decade−1 (95% confidence interval 0.28) over the same period. Increments in lake maximum temperature among the ten lakes range from +0.1 in the west to +1.9 °C decade−1 in the east. Absolute maximum lake surface water temperatures were reached in Wörthersee, 27.5 °C, and Neusiedler See, 31.7 °C. Periods exceeding a critical temperature of 20 °C each year became two to six times longer than the respective average (6 to 93). The depth at which water temperature exceeded 20 °C increased from less than 1 to more than 6 m in Mondsee, Austria, over the 50 years studied. As a consequence, the habitable environment became increasingly restricted for many organisms that are adapted to historic conditions.

Altmetric Badge

Item Type Article
URI https://reading-clone.eprints-hosting.org/id/eprint/100090
Identification Number/DOI 10.1007/s10584-021-03085-1
Refereed Yes
Divisions Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
Publisher Springer
Download/View statistics View download statistics for this item

Downloads

Downloads per month over past year

University Staff: Request a correction | Centaur Editors: Update this record

Search Google Scholar