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The transformed equivalents for original values between the thresholds were calculated assuming a linear relationship.
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In each dataset, its calculation was based on the correlation coefficient between the original values and the values of Y calculated with the model-estimated parameters a and b.
We calculated the ratio of mean absolute error between imputed and original values to the mean value for that variable.
The accuracy of estimation values are calculated by Root Mean Squared error (RMSE) which sum of the different values between imputed and original values and divided by the number of missing values we computed.
The difference between the quantized "representative" value and the original value is called the quantization error.
Any satellites in an orbit between the original value of the semimajor axis of the Moon and the current value would have collided with the Moon and been removed from the system.
The differences between "original" values and "observed" values provide an immediate indication of the storage effect.
Checking this against our original values, 4.4 falls between 3 kPa at 30 °C (86 °F) and 5 kPa at 40 °C (104 °F), and because 37 is closer to 40 than it is to 30, the result should be closer to 5 kPa than it is to 3 kPa.
Third repeat measurements were sometimes close to one of the original values, but as often somewhere in between or far outside the original range.
Next, a two-sided p value was calculated from the proportion of times in which the (absolute) difference computed from the permuted values was greater than the (absolute) difference between original values.
The original values of replication timing (GSE17963_final_data.txt) were scaled between 0 and 1, corresponding to the beginning and the end of the S phase, respectively.
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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