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Reconstructing paleosalinity from δ¹⁸O: Coupled model simulations of the Last Glacial Maximum, Last Interglacial and Late Holocene

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Academic year: 2019

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Table 2: Gradient (αSPACE), intercept (δF) and r2 values from least squares linear regressions on spatial sea surface salinity and δOw data
Table 3: As Table 2 but for temporal relationships. Gradient (αDECADAL), intercept (δF) and r2 values from least squares linear regressions on decadally averaged surfacesalinity and δOw data from the last 100 years of each simulation
FiguresFigure 1: Modelled surface ocean δOc, calculated from the equation of Shackleton (1974)
Figure 2: Regional relationships between spatial sea surface salinity and δpanel shows all observations from the GISS Global Seawater Oxygen-18 Database (Schmidt, 1999b; Bigg and Rohling, 2000,http://data.giss.nasa.gov/o18data/), coloured by degrees latitu
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