Summer temperature gradients in northwest Europe during the Lateglacial to early Holocene transition (15-8 ka BP) inferred from chironomid assemblages.

Peter Langdon, Liam Riddy & Steve Brooks
The raster temperature data was interpolated from site temperature data estimated from Chironomid records using Kriging. Temperatures are in Degrees Centigrage. The dataset covers all of Northern Europe including Iceland and Scandanavia
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