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Late-glacial to late-Holocene shifts in global precipitation 18O

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Figure

Figure 1. The change in surface air temperatures from the last glacial maximum to the preindustrial era (gridded data from Annan andHargreaves, 2013)
Figure 2. Meteoric waterlow temporal resolution of groundwater records means thatvariations within each time period are smoothed and likely repre-sent unequal temporal weighting
Figure 4. Measuredresponds to groundwater and ground ice (circles) or cave calcite(i.e., speleothems; triangles)
Figure 5. Simulated precipitation δ18O differences between the last glacial maximum and pre-industrial time periods (i.e.,δ18Olast glacial maximum – δ18Opre-industrial) from five general circulation models: CAM3iso, ECHAM5-wiso, GISSE2-R, IsoGSM andLMDZ4 (Y
+2

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