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Variability of the ocean heat content during the last millennium – an assessment with the ECHO-g Model

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Academic year: 2021

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Fig. 1. Estimations of the forcing factors used to drive the forced ECHO-G simulations: solar irradiance (red line), greenhouse gas concentrations (green, grey and blue lines for CO 2 , N 2 O and CH 4 , respectively), and the radiative effect of volcanic a
Fig. 2. (a–d) Evolution of OHC700 anomalies normalised per unit area (in 10 8 J m −2 ) in the upper 700 m of the world ocean and the three main ocean basins
Fig. 3. Linear trends of the observed (top panel) and simulated (lower panels) OHC700 (in 10 8 J m −2 yr) in the upper 700 of the ocean for the periods 1955–1990 (left), 1991–2010 (middle) and 2011–2100 (right).
Table 2. Linear trends in OHC700 (in 10 22 J yr −1 ) during the periods 1955–1990 and 1991–2010 in the world ocean, and the three main basins
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