Fig. 6: Variables associated with channelized vertical heat transport for S1 runs.
From: Ice shelf basal channel shape determines channelized ice-ocean interactions
Section-averaged (i.e., \(x\) = 30 and 60 km) across-slope distribution of time-averaged a–d vertical diffusivity and e–h vertical velocity in a, e H60W8, b, f H140W8, c, g H220W8, and d, h H300W8. The ice base in each plot is marked by the pink line, and the planar part of the ice base corresponds to the same ice draft.
