Extended Data Fig. 1: Two-day snapshot and 8-hour zoom of flow conditions at MAVS1.
From: Observations of diapycnal upwelling within a sloping submarine canyon
(a) Potential temperature (θ), (b) turbulent dissipation rate of kinetic energy (ϵ) estimated from the sorting distance when sorting profiles into stable state, (c) buoyancy frequency N calculated from the stable profile, (d) up-canyon velocity and (e) vertical velocity (w) at the MAVS1 mooring.