Fig. 2: Global distribution of the effects of different physical processes on the marine heatwave (MHW) life cycles.
From: Oceanic mesoscale eddies as crucial drivers of global marine heatwaves

Contribution to the \(\left\langle {T}_{a}\right\rangle\) change during the growing phase of the MHWs averaged at each grid point by heat flux convergence of mesoscale eddies (HFC-E) (a) and mean flows (HFC-M) (b), net surface heat flux (NHF) (c), and subgrid-scale mixing (MIX) (d). e–h are the same as a–d, but for the decaying phase of the MHWs. Grids with temporary or permanent sea-ice coverage in the observation are masked by gray.