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In the shallow Baltic Sea, the surface mixed layer depths from the model were typically only a few meters deeper than that observed (Fig. 5b).
Specifically, the models' r-squared scores (the coefficient of determination, which measures the proportion of variability in the data accounted for by the model) were typically in the range 0.20 0.56 when using one Gaussian; 0.73 0.91 with two Gaussians; and 0.91 0.96 with three Gaussians.
When evaluated on the evaluation sets generated with IDFWeight weighting, we observed that the results for each model were typically slightly better compared to the result sets generated with IDFWeight weighting for the following models: RI-Word, RI-Note, RI-Index and W2V (average score gain +3.39%).
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The relaxed model and the proposed OPF model are typically equivalent in transmission systems.
Firstly, concerning verification, a UML model is typically not the input language of a verification tool.
Design spectrum (DS) model is typically specified in a seismic code of practice for structural design.
The parameters of an SEA model are typically derived by considering wave propagation within each subsystem.
The surface air temperature from a numerical model is typically expressed as the temperature at a height of 2 m above the surface.
Similarly, replacing a part of a model with a functionally equivalent part from another model is typically difficult.
The validity of such a model is typically restricted to input signals that are limited in amplitude.
For security software, that model is typically seen as advantageous, because the more people examine a line of code, the more chance there should be of some weakness coming to light.
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