Fig. 2: Evolution of stratification, deep water oxygen concentration and turbulence at a seasonally stratified location in the central Celtic Sea (CTD on Fig. 1) over the summer of 2014.
From: The deepwater oxygen deficit in stratified shallow seas is mediated by diapycnal mixing
a time series of net surface buoyancy forcing. b Evolution of water column temperature. c Deep water O2 concentration. Each point is the average deep water dissolved oxygen concentration. d time series of the rate of dissipation of turbulent kinetic energy (ϵ) at depths of 16 m (blue), 35 m (red), and 47 m (yellow). Source data are provided as a Source Data file.
