Alpine glacier-fed turbid lakes are discontinuous cold polymictic rather than dimictic-Reference-Cited by-同舟云学术

Alpine glacier-fed turbid lakes are discontinuous cold polymictic rather than dimictic

Published:2017-01-02 Issue:1 Volume:7 Page:45-54
ISSN:2044-2041
Container-title:Inland Waters
language:en
Short-container-title:Inland Waters

Author:

Peter Hannes¹²,Sommaruga Ruben¹

Affiliation:

1. Institute of Ecology, Lake and Glacier Ecology Research Group, University of Innsbruck, Innsbruck, Austria

2. Stream Biofilm and Ecosystem Research Laboratory, Faculty of Architecture, Civil and Environmental Engineering, École Polytechnique Fédérale de Lausanne, Lausanne, Switzerland

Funder

Austrian Science Fund

Publisher

Informa UK Limited

Subject

Water Science and Technology,Aquatic Science

Link

https://tandfonline.com/doi/pdf/10.1080/20442041.2017.1294346

Reference50 articles.

1. Variations in the mass-specific absorption coefficient of mineral particles suspended in water

2. Mountain Climates and Climatic Change: An Overview of Processes Focusing on the European Alps

3. Large-scale climatic signatures in lakes across Europe: a meta-analysis

4. Stratification of lakes

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