Efficient Reconstructions of Common Era Climate via Integrated Nested Laplace Approximations
Luis A. Barboza, Julien Emile-Geay, Bo Li, Wan He

TL;DR
This paper demonstrates that integrated nested Laplace approximations (INLA) enable efficient Bayesian inference for paleoclimate reconstructions over the Common Era, confirming human influence on temperature variability with computational advantages over traditional methods.
Contribution
It introduces the application of INLA to paleoclimate modeling, allowing flexible model exploration and efficient inference compared to MCMC, with validation of model choices and data reduction impacts.
Findings
Models with external forcings perform best.
Greenhouse gases are the main driver of temperature changes.
INLA provides faster estimates with comparable accuracy to MCMC.
Abstract
Paleoclimate reconstruction on the Common Era (1-2000AD) provide critical context for recent warming trends. This work leverages integrated nested Laplace approximations (INLA) to conduct inference under a Bayesian hierarchical model using data from three sources: a state-of-the-art prox database (PAGES 2k), surface temperature observations (HadCRUT4), and latest estimates of external forcings. INLA's computational efficiency allows to explore several model formulations (with or without forcings, explicitly modeling internal variability or not), as well as five data reduction techniques. Two different validation exercises find a small impact of data reduction choices, but a large impact for model choice, with best results for the two models that incorporate external forcings. These models confirm that man-made greenhouse gas emissions are the largest contributor to temperature…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsClimate variability and models · Tree-ring climate responses · Plant Water Relations and Carbon Dynamics
