A seasonal-resolution last-millennium reanalysis, built by assimilating climate proxies into an online ocean-atmosphere-sea-ice linear inverse model, matches modern surface-temperature observations as well as annual products while using far fewer proxies.
J., and Coauthors, 2017: Last millennium Northern Hemisphere summer temperatures from tree rings: Part II
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Coupled Seasonal Data Assimilation of Sea Ice, Ocean, and Atmospheric Dynamics over the Last Millennium
A seasonal-resolution last-millennium reanalysis, built by assimilating climate proxies into an online ocean-atmosphere-sea-ice linear inverse model, matches modern surface-temperature observations as well as annual products while using far fewer proxies.