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Alpine glacier-fed turbid lakes are discontinuous cold polymictic rather than dimictic
Glacier retreat as a consequence of climate change influences freshwater ecosystems in manifold ways, yet the physical and chemical bases of these effects are poorly studied. Here, we characterize how water temperature differs between alpine lakes with and without direct glacier influence on seasona...
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Taylor & Francis
2017
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5478930/ https://www.ncbi.nlm.nih.gov/pubmed/28690780 http://dx.doi.org/10.1080/20442041.2017.1294346 |