Table 1 Diapcynal flux estimates are based on the biogeochemical profiles taken on the 19th of June and 21st of August 2014 combined with daily mean ϵ values at the appropriate height (as indicated)
From: The deepwater oxygen deficit in stratified shallow seas is mediated by diapycnal mixing
Date | Name (ϵ depth) | Flux |
|---|---|---|
19/06 | NO2 + NO3(36 m) | 2.8 ± 0.7 m mol m−2d−1 |
DIC(36 m) | 20.8 ± 5.4 m mol m−2d−1 | |
O2 up (16 m) | 45.9 ± 14.1 m mol m−2d−1 | |
O2 down (47 m) | − 4.0 ± 1.2 m mol m−2d−1 | |
21/08 | NO2 + NO3(36 m) | 1.9 ± 0.5 m mol m−2d−1 |
DIC(36 m) | 10.8 ± 2.8 m mol m−2d−1 | |
O2 up (36 m) | 6.5 ± 1.7 m mol m−2d−1 | |
O2 down (47 m) | − 20.2 ± 6.0 m mol m−2d−1 |
