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Fig. 4 | Progress in Earth and Planetary Science

Fig. 4

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. 4

a The thermosteric sea level change ∆ηθ (cm), b thermosteric sea level change due to TR (∆ηTR), and c thermosteric sea level change due to TA (∆ηTA) for years 51–70 in the faf-heat experiment of MIROC6, and d the thermosteric sea level change due to TA (∆ηTA) for years 51–70 in the passive-heat experiment of MIROC6. Note that deviations from the basin average in the North Pacific are depicted in the figures. Areas with signals at a 90% confidence level are hatched in a. Note that the basin average in the North Pacific is subtracted from the thermosteric sea level change at each grid. Contours indicate the climatological DSL in piControl

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