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Fuzzy membership values were derived from landslide frequency ratio.
Natural resource values were derived from various sources.
Gated (step function) values were derived from the true curves; CMI values were derived from gated values and evaluated.
Approximately equal CTMI parameter values were derived irrespective of the temperature region, except for Tmax.
We used the standard curve quantification method that absolute values were derived from known quantities.
*p values were derived using Wilcoxon signed-rank test (*p < 0.05).
Similar(6)
Again, permutation-based p-values were derived.
Corresponding p-values were derived from the theoretical t-distributions.
The non-null z-values were derived from their corresponding exponentially distributed Vg.
Corresponding p-values were derived.
P-values were derived from two-sided tests.
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