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Hockey Stick? What Hockey Stick? - WEBCommentary

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Lomonosovfonna Ice Core, Svalbard, Norway<br />

Grinsted et al. (2006), from data obtained from a 121-meter-long ice core extracted from the highest ice<br />

field in Svalbard (Lomonosovfonna: 78°51'53"N, 17°25'30"E), developed "a model of chemical<br />

fractionation in ice based on differing elution rates for pairs of ions ... as a proxy for summer melt<br />

(1130-1990)," which was "validated against twentieth-century instrumental records and longer<br />

historical climate proxies." This work revealed, in their words, that "the Medieval Warm Period in<br />

Svalbard summer conditions [was] as warm (or warmer) as present-day," because "the degree of<br />

summer melt was significantly larger during the period 1130-1300 than in the 1990s."<br />

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