Fig. 5: Ocean heat flux divergence.
From: Seafloor roughness reduces melting of East Antarctic ice shelves
Divergence of time-averaged, vertically-integrated total ocean heat fluxes in (W m−2) from (a) the BedMachine simulation and (b) the SRTM15 simulation. Negative divergence corresponds to convergence (source) of ocean heat fluxes. c Difference in magnitude of the energy convergence in (W m−2) between the SRTM15 and BedMachine simulations. (thin black) Ice shelf boundary and (thick black) 1000 m isobath.
