1
The IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0–55 cal kBP)
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Marine20—The Marine Radiocarbon Age Calibration Curve (0–55,000 cal BP)
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SHCal20 Southern Hemisphere Calibration, 0–55,000 Years cal BP
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Dynamic time warping of palaeomagnetic secular variation data
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Heteroscedastic Gaussian Process Regression on the Alkenone over Sea Surface Temperatures
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A library of early Cambrian chemostratigraphic correlations from a reproducible algorithm
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Data Constraints on Glacial Atlantic Water Mass Geometry and Properties
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Fast and Stable Multivariate Kernel Density Estimation by Fast Sum Updating
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Multivariate Gaussian and Student-t process regression for multi-output prediction
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Regional and global benthic δ18O stacks for the last glacial cycle
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Understanding Probabilistic Sparse Gaussian Process Approximations
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Times Series Averaging and Denoising from a Probabilistic Perspective on Time–Elastic Kernels
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Dynamic Time Warping Averaging of Time Series Allows Faster and More Accurate Classification
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A Late Pleistocene sea level stack
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Termination 1 timing in radiocarbon‐dated regional benthic δ18O stacks
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Probabilistic sequence alignment of stratigraphic records
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Phasing of millennial climate events and northeast Atlantic deep-water temperature change since 50 ka BP
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Gaussian processes for time-series modelling
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Independent Doubly Adaptive Rejection Metropolis Sampling Within Gibbs Sampling
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The Mean Age of Ocean Waters Inferred from Radiocarbon Observations: Sensitivity to Surface Sources and Accounting for Mixing Histories
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Flexible paleoclimate age-depth models using an autoregressive gamma process
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The timing of deglacial circulation changes in the Atlantic
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Variational Heteroscedastic Gaussian Process Regression
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Testing the impact of seasonal phytodetritus deposition on δ13C of epibenthic foraminifer Cibicidoides wuellerstorfi: A 31,000 year high‐resolution record from the northwest African continental slope
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A global averaging method for dynamic time warping, with applications to clustering
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Bipolar seesaw in the northeastern tropical Atlantic during Heinrich stadials
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MEME Suite: tools for motif discovery and searching
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Variational Learning of Inducing Variables in Sparse Gaussian Processes
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Sahel megadroughts triggered by glacial slowdowns of Atlantic meridional overturning
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Coherent high- and low-latitude control of the northwest African hydrological balance
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A simple monotone process with application to radiocarbon‐dated depth chronologies
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Markov Chain Monte Carlo: Stochastic Simulation for Bayesian Inference
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Most likely heteroscedastic Gaussian process regression
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Fast particle smoothing: if I had a million particles
35
Gaussian Processes for Machine Learning (Adaptive Computation and Machine Learning)
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Heteroscedastic Gaussian process regression
37
Radiocarbon peat chronologies and environmental change
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An Atlantic lead over Pacific deep-water change across Termination I: implications for the application of the marine isotope stage stratigraphy
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A Pliocene‐Pleistocene stack of 57 globally distributed benthic δ18O records
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Absolute calibration of the Greenland time scale: implications for Antarctic time scales and for Δ14C
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Rapid transient changes in northeast Atlantic deep water ventilation age across Termination I
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Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes
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Radiocarbon calibration beyond 20,000 14C yr B.P. by means of planktonic foraminifera of the Iberian Margin
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Millennial‐scale variability of deep‐water temperature and δ18Odw indicating deep‐water source variations in the Northeast Atlantic, 0–34 cal. ka BP
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Variable kernel density estimation
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Sequential Monte Carlo Methods in Practice
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Application of dynamic programming to the correlation of paleoclimate records
48
The Salinity, Temperature, and δ18O of the Glacial Deep Ocean
49
Statistical Methods in Bioinformatics: An Introduction
50
Probabilistic Models For Joint Clustering And Time-Warping Of Multidimensional Curves
51
Spoken Language Processing: A Guide to Theory, Algorithm and System Development
52
Phase relationships between millennial‐scale events 64,000–24,000 years ago
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Hydrological relationship between the North Atlantic Ocean and the Mediterranean Sea during the past 15‐75 kyr
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Continuous dynamic time warping for translation-invariant curve alignment with applications to signature verification
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Biological Sequence Analysis: Probabilistic Models of Proteins and Nucleic Acids
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Changes in east Atlantic deepwater circulation over the last 30
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Patterns of ice-rafted detritus in the glacial North Atlantic (40–55°N)
58
Speaker-independent continuous-speech recognition by phoneme-based word spotting and time-synchronous context-free parsing☆
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On the hidden Markov model and dynamic time warping for speech recognition — A unified view
60
Bayesian Analysis of the Two-Parameter Gamma Distribution
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Maximum likelihood from incomplete data via the EM - algorithm plus discussions on the paper
62
The DRAGON system--An overview
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Monte Carlo Sampling Methods Using Markov Chains and Their Applications
64
A general method applicable to the search for similarities in the amino acid sequence of two proteins.
65
Regional and global benthic 18 O stacks for the last glacial cycle
66
Machine learning - a probabilistic perspective
67
Interhemispheric symmetry of the tropical African rainbelt over the past 23,000 years
68
A New Robust Statistical Model for Radiocarbon Data
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The Application of Hidden Markov Models in Speech Recognition
70
Abrupt onset and termination of the African Humid Period:rapid climate responses to gradual insolation forcing
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Profile hidden Markov models
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Bayesian Inference in Statistical Analysis of Paleoclimate Records . PhD thesis, Brown University, 2016. [6] S. R. Eddy. Profile hidden markov models
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A Compendium of Conjugate Priors
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Speaker-Independent English Consonant and Japanese Word Recognition by a Stochastic Dynamic Time Warping Method
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LGM (red) Southern Sourced Water (SSW) percentages for the seven cores analyzed in the study
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36 17 Dual proxy age inferences and alignments of SU90-08 to DNA stack. This figure also shows how multiple observations at the same depths are dealt with in the alignment algorithm
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Un-shifted δ 18 O records for SU90-08 (red) and GeoB9526-5 (blue) aligned to the DNEA stack (grey)
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13 (a) Two sets of input-output pairs, colored red and blue, are picked asynchronously from the same signal. (b) Two true signals to be aligned, which are designed to be identical