Heteroscedastic Gaussian Process Regression on the Alkenone over Sea Surface Temperatures

To restore the historical sea surface temperatures (SSTs) better, it is important to construct a good calibration model for the associated proxies. In this paper, we introduce a new model for alkenone (${\rm{U}}_{37}^{\rm{K}'}$) based on the heteroscedastic Gaussian process (GP) regression method. Our nonparametric approach not only deals with the variable pattern of noises over SSTs but also contains a Bayesian method of classifying potential outliers.

Dual Proxy Gaussian Process Stack: Integrating Benthic $δ^{18}{\rm{O}}$ and Radiocarbon Proxies for Inferring Ages on Ocean Sediment Cores

Ages in ocean sediment cores are often inferred using either benthic ${\delta}^{18}{\rm{O}}$ or planktonic ${}^{14}{\rm{C}}$ of foraminiferal calcite. Existing probabilistic dating methods infer ages in two distinct approaches: ages are either inferred directly using radionuclides, e.g. Bacon [Blaauw and Christen (2011)]; or indirectly based on the alignment of records, e.g. HMM-Match [Lin et al. (2014)]. In this paper, we introduce a novel algorithm for integrating these two approaches by constructing Dual Proxy Gaussian Process (DPGP) stacks, which represent a probabilistic model of benthic ${\delta}^{18}{\rm{O}}$ change (and its timing) based on a set of cores. While a previous stack construction algorithm, HMM-Match, uses a discrete age inference model based on Hidden Markov models (HMMs) [Durbin et al. (1998)] and requires a number of records enough to sufficiently cover all its ages, DPGP stacks with time-varying variances are constructed with continuous ages obtained by particle smoothing [Doucet et al. (2001); Klaas et al. (2006)] and Markov-chain Monte Carlo (MCMC) [Peters (2008)] algorithms, and can be derived from a small number of records by applying the Gaussian process regression [Rasmussen and Williams (2005)]. As an example of the stacking method, we construct a local stack from 6 cores in the deep northeastern Atlantic Ocean and compare it to a deterministically constructed ${\delta}^{18}{\rm{O}}$ stack of 58 cores from the deep North Atlantic [Lisiecki and Stern (2016)]. We also provide two examples of how dual proxy alignment ages can be inferred by aligning additional cores to the stack.