Hyperpycnal flows control the persistence and flushing of hypoxic high-conductivity bottom water in a High Arctic lake
In the deepest portions of many lakes, zones of high-conductivity bottom water (HCBW) depleted in dissolved oxygen (DO) are present. HCBW and DO are important for determining benthic diversity and abundance, nutrients, and contaminant cycling and understanding the long-term evolution of lakes. We in...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Canadian Science Publishing
2018-12-01
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| Series: | Arctic Science |
| Subjects: | |
| Online Access: | https://doi.org/10.1139/as-2017-0022 |