Winter Temperature Eurasian Data Assimilation Reconstruction (WinTEDA)

A winter, 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 and Greenland paleoclimate data that have a correlation with winter temperature (p < 0.05, accounting for proxy autocorrelation). The reconstruction also includes long observational temperature records from the Northern Hemisphere.