Fig. 4: Modeled thermocline depth.
From: Observational evidence for on-shelf heat transport driven by dense water export in the Weddell Sea
Mean thermocline depth along the 1000-m isobath for winter runs using the idealized model described by Daae et al.22 with (red line, Dense) and without (blue line, No Dense) dense water outflow from the idealized Filchner Trough. The position of the trough is marked in grey shadings, and the envelopes give the standard deviation (std).
