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If the interest is in comparing β i to a particular value, you can simply give the posterior probability that β i falls in any particular range of values.
Because control of factors changing across strata is no longer achieved by design, in addition to the regressors x i we also include stratum indicator variables (a vector z i ): 2 It helps understand the conditional variant of this model to re-write the term α T z i as αs where day i falls in stratum s (thus vector α = (α1,…, αS)).
The predicted or fitted values for CD and SB were computed as: (8) where the probability that observation i falls in category c was calculated as: (9) Above, Φ is the cumulative distribution function of a standard normal variate; τc is the assumed (or estimated) value of the appropriate threshold for CD and SB, and is the posterior mean of the liability to CD or SB for individual i.
Zone I falls in a rock-domain, while zones II to VI are observed from a domain of evaporation.
In this case, we define that each value in our plot assumes a value of τmax=0.0625 i, where i falls in the interval from 1 to 8 that is used in the evaluation of each protocol's time slot parameter.
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Since I tried Ludwig back in 2017, I have been constantly using it in both editing and translation. Ever since, I suggest it to my translators at ProSciEditing.

Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com