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Water isotopes – climate relationships for the mid-Holocene and preindustrial period simulated with an isotope-enabled version of MPI-ESM

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Academic year: 2020

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Figure

Table 1. Selected ice core records and their geographical coordinates, reported PI values of δ18O and d-excess, and changes in δ18O andd-excess between 6k and PI
Figure 1. (a)bothtemperatures are below Global distribution of simulated (background pattern) and observed (colored markers; see text for details) annual mean δ18Opvalues in precipitation under PI conditions
Figure 2. (a)of observed vs. modeled(mean over the first 10 m of depth) under PI conditions with observed Comparison of the global distribution of simulated (background pattern) annual mean δ18Ooce values in ocean surface water δ18Ooce values of the GISS da
Figure 3. Scatter plots ofsalinity for the δ18O in ocean surface water vs. surface (a) Atlantic, (b) Pacific, (c) Indian, (d) Southern and(e) Arctic Ocean under PI conditions
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