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If we use Γ C = Γ ∖ Γ E = Γ D ∪ Γ F instead of Γ D in (4) and (5) and set the permittivities ε correctly, the model with a high relative permittivity ε F is the special case (1 - 6) of the full model (1 - 8) with a floating potential.
By capturing the short timescale correctly, the model assures the credibility of the longer timescale.
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For instance, correctly identifying the model input parameter values is a daunting task.
Relative predictions, representing the spatial variability in sediment exports, were correctly represented by the model.
These suggest that the main factors involved have been correctly incorporated into the model.
However, some specific borders, e.g. the Appalachian rim, are correctly reproduced in the model.
c Percent of samples correctly classified by the model.
The RMSEA indicates the proportion of variance-covariance information not correctly predicted by the model.
The percent of admissions correctly classified by the model were also calculated.
Our results indicate that under the correctly specified model, ignoring the sample weights does not affect the results.
Using the model-robust approach, we see no inflation in the correctly specified model (Figure 1), or for either of the mis-specified models (Figure 2).
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