Fig. 3: Kinetic energy of the ocean circulation.
From: Seafloor roughness reduces melting of East Antarctic ice shelves
a, b, c Time-averaged kinetic energy integrated over top 1000 m in log10(J m−2) from the BedMachine simulation and (d, e, f) from the SRTM15 simulation. g, h, i Kinetic energy difference in (J m−2) between the SRTM15 and BedMachine simulations. (a, d, g) Mean, (b, e, h) seasonal, and (c, f, i) eddy kinetic energy components. (thin black) Ice shelf boundary, (thick black) 1000 m isobath, and (thin grey) vertically-integrated transport in (Sv) are shown.
