Extended Data Fig. 3: Probability density functions (PDF) and time series of the terms in the volume budget below a temperature surface.
From: Observations of diapycnal upwelling within a sloping submarine canyon
![Extended Data Fig. 3](https://cdn.statically.io/img/media.springernature.com/full/springer-static/esm/art%3A10.1038%2Fs41586-024-07411-2/MediaObjects/41586_2024_7411_Fig7_ESM.jpg)
(a) PDFs of the depth-averaged in-flow (\({u}_{in}\tan \alpha \)) estimated from along-canyon velocities below 3. 7 °C at MP1 (blue) and below 4. 2 °C at MP2 (red) and the depth-averaged adiabatic vertical velocity (\({w}_{adia}=\frac{d\eta }{dt}\), where η is the isotherm displacement) at MP1 (green) and MP2 (orange). The range of values of wdye are shown by the grey shaded region. (b) Time series of \({u}_{in}\tan \alpha \) (red) and wadia (orange) from MP2. The range of values of wdye are shown by the grey shaded region.