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    MathWorks Inc mcmc method
    Mcmc Method, supplied by MathWorks Inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
    https://www.bioz.com/product/mcmc+method/pm34889482-360-3-1
    Average 90 stars, based on 1 article reviews
    mcmc method - by Bioz Stars, 2026-10
    90/100 stars

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    Comparison:

    Article Title: Nonparametric Bayes testing of changes in a response distribution with an ordinal predictor
    Article Snippet: For example, it took approximately 33 hours to complete the MCMC for our analysis of the comet assay data using a Matlab (version 7.1) program compiled in C and run on a Dell Optiplex SX270 (2.8 GHz Pentium 4 processor).

    Article Title: Social Contagion and General Diffusion Models of Adolescent Religious Transitions: A Tutorial, and EMOSA Applications.
    Article Snippet: Epidemic Models of the Onset of Social Activities (EMOSA) describe behaviors that spread through social networks.. Two social influence methods are represented, social contagion (one-to-one spread) and general diffusion (spread through cultural channels).. Past models explain problem behaviors—smoking, drinking, sexuality, and delinquency.

    Article Title: An analysis on the structural stability of Okun's law--a cross-country study
    Article Snippet: Taylor & Francis makes every effort to ensure the accuracy of all the information (the “Content”) contained in the publications on our platform.. However, Taylor & Francis, our agents, and our licensors make no representations or warranties whatsoever as to the accuracy, completeness, or suitability for any purpose of the Content.. Any opinions and views expressed in this publication are the opinions and views of the authors, and are not the views of or endorsed by Taylor & Francis.

    Article Title: Mathematical Modeling and Simulation of 1,3-Propanediol Production by Klebsiella pneumoniae BLh-1 in a Batch Bioreactor Using Bayesian Statistics.
    Article Snippet: Mathematical modeling and computer simulation are fundamental for optimizing biotechnological processes, enabling cost reduction and scalability, thereby driving advancements in the bioindustry.. In this work, mathematical modeling and estimation of fermentative kinetic parameters were carried out to produce 1,3‐propanediol (1,3‐PDO) from residual glycerol and Klebsiella pneumoniae BLh‐1.. The Markov chain Monte Carlo method, using the Metropolis‐Hastings algorithm, was applied to experimental data from a batch bioreactor under aerobic and anaerobic conditions.

    Article Title: Probe-level measurement error improves accuracy in detecting differential gene expression.
    Article Snippet: The MCMC method is implemented in Matlab.

    Article Title: Forecasting risk via realized GARCH, incorporating the realized range
    Article Snippet: The RG-GG model is fit to each data-set from Model 1, once using the MCMC method and once using the ML estimator, the latter employing the ‘fmincon’ constrained optimization routine in Matlab software.



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    Flow chart of the method used to impute the missing solutions within and between Gravity Recovery and Climate Experiment and its Follow On (GRACE (‐FO)) missions. First, the informative priors were derived from the GRACE (‐FO) for a single grid point/basin time series as the ranges of the intercepts, slopes, variability, amplitudes, and frequencies of the annual and semiannual cycles in the GRACE (‐FO) time series, assuming an additive generative model describing the geophysical signal in GRACE data as long‐term variability (secular trend + interannual to decadal variability), annual, and semi‐annual. Second, we combined the likelihood data and the priors in the Markov Chain Monte Carlo sampling to generate posterior distributions for each of the component storages. Third, we merged the median of the posteriors for the component storages to reconstruct the full GRACE (‐FO) total water storage and its uncertainty at 95% credible interval. We added the residuals back to the observed time series to preserve the same variability as the original GRACE time series. We applied 5‐fold cross validations to validate the model internally and generate a predictive posterior distribution that can be used to infer the present and near future of the total signal.
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    Flow chart of the method used to impute the missing solutions within and between Gravity Recovery and Climate Experiment and its Follow On (GRACE (‐FO)) missions. First, the informative priors were derived from the GRACE (‐FO) for a single grid point/basin time series as the ranges of the intercepts, slopes, variability, amplitudes, and frequencies of the annual and semiannual cycles in the GRACE (‐FO) time series, assuming an additive generative model describing the geophysical signal in GRACE data as long‐term variability (secular trend + interannual to decadal variability), annual, and semi‐annual. Second, we combined the likelihood data and the priors in the Markov Chain Monte Carlo sampling to generate posterior distributions for each of the component storages. Third, we merged the median of the posteriors for the component storages to reconstruct the full GRACE (‐FO) total water storage and its uncertainty at 95% credible interval. We added the residuals back to the observed time series to preserve the same variability as the original GRACE time series. We applied 5‐fold cross validations to validate the model internally and generate a predictive posterior distribution that can be used to infer the present and near future of the total signal.

    Journal: Earth and Space Science (Hoboken, N.j.)

    Article Title: Reconstruction of GRACE Mass Change Time Series Using a Bayesian Framework

    doi: 10.1029/2021EA002162

    Figure Lengend Snippet: Flow chart of the method used to impute the missing solutions within and between Gravity Recovery and Climate Experiment and its Follow On (GRACE (‐FO)) missions. First, the informative priors were derived from the GRACE (‐FO) for a single grid point/basin time series as the ranges of the intercepts, slopes, variability, amplitudes, and frequencies of the annual and semiannual cycles in the GRACE (‐FO) time series, assuming an additive generative model describing the geophysical signal in GRACE data as long‐term variability (secular trend + interannual to decadal variability), annual, and semi‐annual. Second, we combined the likelihood data and the priors in the Markov Chain Monte Carlo sampling to generate posterior distributions for each of the component storages. Third, we merged the median of the posteriors for the component storages to reconstruct the full GRACE (‐FO) total water storage and its uncertainty at 95% credible interval. We added the residuals back to the observed time series to preserve the same variability as the original GRACE time series. We applied 5‐fold cross validations to validate the model internally and generate a predictive posterior distribution that can be used to infer the present and near future of the total signal.

    Article Snippet: We then used the MCMC method to generate 2,000 samples from the posterior distribution ( P ( θ | D ) for each component (Durbin & Koopman, ; Harvey, ; Scott & Varian, ) (Figure ).

    Techniques: Derivative Assay, Sampling

    Modeled total water storage during the Gravity Recovery and Climate Experiment (GRACE) and GRACE‐Follow On gap as the sum of the median posterior distribution of long‐term variability (variability ≥12‐month, including secular trend and interannual‐decadal variations), annual and semi‐annual signals between April 2002 and April 2021, sampled from 2,000 steps using Markov Chain Monte Carlo with the No‐U‐Turn Sampling method. Uncertainties associated with these signals are provided in supplementary materials at 5% and 95% levels (Figures S2, S3 in Supporting Information  ).

    Journal: Earth and Space Science (Hoboken, N.j.)

    Article Title: Reconstruction of GRACE Mass Change Time Series Using a Bayesian Framework

    doi: 10.1029/2021EA002162

    Figure Lengend Snippet: Modeled total water storage during the Gravity Recovery and Climate Experiment (GRACE) and GRACE‐Follow On gap as the sum of the median posterior distribution of long‐term variability (variability ≥12‐month, including secular trend and interannual‐decadal variations), annual and semi‐annual signals between April 2002 and April 2021, sampled from 2,000 steps using Markov Chain Monte Carlo with the No‐U‐Turn Sampling method. Uncertainties associated with these signals are provided in supplementary materials at 5% and 95% levels (Figures S2, S3 in Supporting Information ).

    Article Snippet: We then used the MCMC method to generate 2,000 samples from the posterior distribution ( P ( θ | D ) for each component (Durbin & Koopman, ; Harvey, ; Scott & Varian, ) (Figure ).

    Techniques: Sampling

    [a] Markov Chain Monte Carlo regression model diagnostic test with coefficient of determination (r 2 ). [b] Empirical cumulative density function (ecdf) for r 2 showing ≥80% of the grid cells have r 2 ≥ 58%. Variabilities in the predictable signal and the residuals are provided in SI (Figure S5 in Supporting Information  ).

    Journal: Earth and Space Science (Hoboken, N.j.)

    Article Title: Reconstruction of GRACE Mass Change Time Series Using a Bayesian Framework

    doi: 10.1029/2021EA002162

    Figure Lengend Snippet: [a] Markov Chain Monte Carlo regression model diagnostic test with coefficient of determination (r 2 ). [b] Empirical cumulative density function (ecdf) for r 2 showing ≥80% of the grid cells have r 2 ≥ 58%. Variabilities in the predictable signal and the residuals are provided in SI (Figure S5 in Supporting Information ).

    Article Snippet: We then used the MCMC method to generate 2,000 samples from the posterior distribution ( P ( θ | D ) for each component (Durbin & Koopman, ; Harvey, ; Scott & Varian, ) (Figure ).

    Techniques: Diagnostic Assay