Winter Temperature Eurasian Data Assimilation Reconstruction (WinTEDA)

<p>A winter,&nbsp;Eurasian-focused paleoclimate temperature reconstruction over the past 1000 years. The reconstruction is over a seasonal average of December to February. The reconstruction includes Eurasia&nbsp;and Greenland paleoclimate data that have a correlation with winter temperature (p &lt; 0.05, accounting for proxy autocorrelation). The reconstruction also includes long observational temperature records from the Northern Hemisphere.</p>