Fig. 5 | Nature Communications

Fig. 5

From: Low ocean-floor rises regulate subpolar sea surface temperature by forming baroclinic jets

Fig. 5The alternative text for this image may have been generated using AI.

Barotropic ambient potential vorticity and barotropic streamfunction. Contour lines denote barotropic ambient potential vorticity f/H (contour interval: 5 × 10−10 s−1 m−1) and shade denotes streamfunction derived from the JCOPE2 reanalysis. Closed contours of f/H are present over the rises A, A′, and C

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