Fig. 7
From: Low ocean-floor rises regulate subpolar sea surface temperature by forming baroclinic jets
Barotropic streamfunction and a jet formation in a western North Pacific simulation. Temporal mean field of barotropic streamfunction (color shade; ×106 m3 s−1) and surface current at a depth of 12 m (vector, cm s−1) of the Meteorological Research Institute Community Ocean Model (MRI.COM)32,33 are indicated. The simulation exhibits anticyclonic barotropic flow over the rise A and the Isoguchi J1. Model configurations are described in Methods
