Fig. 5
From: Deep-ocean mixing driven by small-scale internal tides
Geography of the ratio q of local energy dissipation to total energy conversion. The ratio q is here defined as \(q = E_{{\mathrm{M}}_2}^{4 - \infty }/E_{{\mathrm{M}}_2}^{1 - \infty }\), and is binned in 2° × 2° squares for visual purposes. Inset bar-plot represents histograms of (black) seafloor area and (white) \(E_{{\mathrm{M}}_2}^{1 - \infty }\) binned as a function of q, and error bars represent the 25th and 75th percentiles on both sides of the median (square)
