Fig. 6
From: Ocean convection linked to the recent ice edge retreat along east Greenland
Observed and modelled hydrographic profiles. Profile from the August 2012 cruise modified to have a uniform 80 m deep mixed layer (in grey/black) that was closest to the February 2016 glider’s western turnaround point (profile in blue). The red profile is the result of a simulation by the one-dimensional PWP model using the modified summertime profile as initial conditions and forced by a constant heat loss of 120 W/m2 from November to mid-February
