Glacial cooling and climate sensitivity revisited

Assimilating sea surface temperature proxies over the Last Glacial Maximum constrains equilibrium climate sensitivity.

Resolving the differences in the simulated and reconstructed climate response to volcanism over the last millennium

Assimilating tree-ring records helps resolve discrepancies between simulated and reconstructed climate reponse to volcanism.

A data assimilation approach to last millennium temperature field reconstruction using a limited high-sensitivity proxy network

We reconstruct Nothern Hemisphere temperatures over the last millennium by assimilating a highly-sensitive, curated tree-ring network.

Globally resolved surface temperatures since the Last Glacial Maximum

We reconstruct surface temperatures since the Last Glacial Maximum using data assimilation.