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Comparing proxy and model estimates of hydroclimate variability and change over the Common Era

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Figure

Figure 1. Annual reconstructions of seawatertion), Palmyra (Nurhati et al., 2011b, 2016), Fiji (Linsley et al., 2004, 2006; Linsley, 2017a), Great Barrier Reef (Hendy et al., 2002, 2017)(pentannual resolution), Rarotonga (Linsley et al., 2000; Ren et al.,
Figure 2. The slope of the multitaper spectrum expressed as β value (Huybers and Curry, 2006) for climate and tree-ring variables atlocations with tree-ring chronologies from the North American Drought Atlas (Cook et al., 1999, 2010b), the Monsoon Asia Dro
Figure 3. Examples of the effect of age model uncertainty and spectral reddening on paleoclimate signatures in sedimentary archives.model uncertainty associated with the Lake Naivasha (East Africa) lake level record (Verschuren et al., 2000) spanning the l
Figure 4. The amount of climatic information extracted from Chi-nese classical documents (a reproduction of Fig
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