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Progress in Earth and Planetary Science
Fig. 2 | Progress in Earth and Planetary Science

Fig. 2

From: Future dynamic sea level change in the western subtropical North Pacific associated with ocean heat uptake and heat redistribution by ocean circulation under global warming

Fig. 2

Dynamic sea level changes (cm) for years 51–70 relative to piControl for a faf-stress, b faf-heat, and c faf-stress experiments of MIROC6. The contours in the upper panels indicate the climatological dynamic sea level in piControl. Regions with signals at a 90% confidence level are hatched. The middle panels show the heat flux change ΔQSST (Wm−2) for years 1–70 relative to piControl for d faf-stress, e faf-heat, and f faf-stress experiments of MIROC6. The contour indicates the climatological net heat flux into the ocean in piControl. The lower panels (g–i) are same as the upper panels, but for the ensemble mean of three members of MIROC5.2. Areas in which the signs of the three members do not agree were masked out

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