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Modelling circulation in an ice-covered lake
In deep ice-covered lakes with temperatures below 4 °C the heat flux from the bottom sediment results in a horizontal density gradient and a consequent flow along the bottom slope. Measurements in Lake Pääjärvi, Finland, show a stable temperature field where a heat gain through the bottom and a heat...
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| Main Authors: | , , , , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Estonian Academy Publishers
2010-12-01
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| Colecção: | Estonian Journal of Earth Sciences |
| Assuntos: | |
| Acesso em linha: | http://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2010/issue_4/earth-2010-4-298-309.pdf |
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