Gas transfer velocity (k600) increases with discharge in steep streams but not in low‐slope streams
Abstract Gas transfer velocity (k600) controls gas fluxes between aquatic ecosystems and the atmosphere. In streams, k600 is controlled by turbulence and, thus, local hydrology and geomorphology. Resultantly, variability in k600 can be large and modeling k600 from physical parameters can have large...
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| Main Authors: | , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Wiley
2025-06-01
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| Series: | Limnology and Oceanography Letters |
| Online Access: | https://doi.org/10.1002/lol2.70003 |
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