Hemispheric mean temperatures that have been reconstructed with a wide range of climate proxies indicate that temperatures were warmer in Medieval times than during the subsequent “Little Ice Age” (∼1550 to 1850) ([1][1]). However, all studies of large-scale climate variations reveal some regions that do not follow the global or hemispheric trend [for example, ([2][2])], so selecting a few data points, as W. S. Broecker does in his Perspective ( Science 's Compass, 23 Feb., p. [1497][3]), adds little to resolving the title question he poses: “Was the Medieval Warm Period global.” Furthermore, Broecker's statement that only borehole temperatures and snowlines can reconstruct temperatures to within 0.5_C is not supported in the literature. Reconstructing global temperature requires a geographically extensive network of data. Studies that have analyzed data from a wider range of instruments than Broecker mentions ([1][1], [3][4]) conclude that 20th century warming is unprecedented, in both rate and magnitude, compared with warming during the past 1000 years. Medieval climate was clearly unusual in some areas ([4][5]), and further regional studies are needed. These might help determine if Broecker's hypothesis of a change in thermohaline circulation holds water. 1. [↵][6]1. P. D. Jones 2. et al ., Holocene 8, 455 (1998); 1. M. E. Mann, 2. R. S. Bradley, 3. M. K. Hughes , Geophys. Res. Lett. 26. 2. [↵][7]1. T. J. Crowley, 2. T. S. Lowery , Ambio 29, 1999 (2000) 759;51. 3. [↵][8]1. P. D. Jones , et al., Rev. Geophys. 37, 173 (1999). 4. [↵][9]1. M. K. Hughes, 2. H. F. Diaz , Clim. Change 26, 109 (1996); 1. K. R. Briffa 2. et al ., J. Geophys. Res. 106D, 2929 (2001). 5. 1. A.S. Issar, 2. N. Brown 1. S. Stine , in Water, Environment and Society in Times of Climatic Change, A.S. Issar, N. Brown, Eds. (Kluwer, Dordrecht, Netherlands, 1998), pp. 43-67; 1. M. K. Hughes, 2. G. Funkhauser , in The Impacts of Climate Variability on Forests, M. Beniston, J.L. Innes, (Springer-Verlag, Berlin, 1998, pp. 99–107; 1. C. Pfister 2. et al ., Holocene 8, 535 (1998); 1. V. C. LaMarche , Science 183, 1043 (1974); 1. D. Dahl-Jenssen 2. et al ., Science 282, 268 (1998). [1]: #ref-1 [2]: #ref-2 [3]: /lookup/doi/10.1126/science.291.5508.1497 [4]: #ref-3 [5]: #ref-4 [6]: #xref-ref-1-1 View reference 1 in text [7]: #xref-ref-2-1 View reference 2 in text [8]: #xref-ref-3-1 View reference 3 in text [9]: #xref-ref-4-1 View reference 4 in text
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