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        <gco:CharacterString>STUDY NOTES: Data tables are provided, linked directly to the three figures shown in the publication. The figure captions provide the necessary description of the data. Fig. 1: The 14 temperature-related proxy records used in this study, filtered to remove variations on time scales less than 20 years and then normalised to have zero mean and unit standard deviation during the period from 800 to 1995 [with adjustments made to the shorter records]. Fig. 2. Fraction of the records available in each year that have normalized values &gt; 0, &gt; 1, &gt; 2, &lt; 0, &lt; -1, and &lt; -2, with the latter three series multiplied by –1. The series are shown from 800 to 1995 and have been filtered to remove variations on time scales less than 20 years. Fig. 3. Difference between the fraction of the records available in each year that have normalized values (A) &gt; 0 and &lt; 0, (B) &gt; 1 and &lt; -1, (C) &gt; 2 and &lt; -2, and (D) as (A) but using a shorter (1865 to 1995) reference period for normalization. The difference series are shown for 800 to 1995 and have been filtered to remove variations on time scales less than 20 years. Zero indicates that the number of series exceeding the upper threshold equals those with values below the lower threshold. In (D), results based on annual-mean instrumental temperatures from grid boxes throughout the NH (red curve) or only in regions close to the proxy records (green curve) are shown for 1856 to 2004 (also normalized over the period from 1856 to 1995). LAST UPDATE: 2/2006 (Addition of Fig. 1 raw series) 
ABSTRACT SUPPLIED BY ORIGINATOR: Periods of widespread warmth or cold are identified by positive or negative deviations that are synchronous across a number of temperature-sensitive proxy records drawn from the Northern Hemisphere. The most significant and longest duration feature during the last 1200 years is the geographical extent of warmth in the middle to late 20th century. Positive anomalies during 890 to 1170 and negative anomalies during 1580 to 1850 are consistent with the concepts of a Medieval Warm Period and a Little Ice Age, but comparison with instrumental temperatures shows the spatial extent of recent warmth to be of greater significance than that during the medieval period.</gco:CharacterString>
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