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There is a need for a better algorithm than the above mentioned adjacency vector based one, which can take more realistic parameter (e.g. subject's varying speed), and requires lesser space.
Therefore, while the single- and two-target cell models each provide good fits which are well supported by the data, the two target cell model does so under more realistic parameter values, suggesting that it offers a better description of the dynamics.
McClelland et al.[ 6] showed that this multiple imputation technique yields more realistic parameter estimates than other traditional approaches to missing data.
For the other (arguably more realistic) parameter combinations, precision of the LD method was higher, and often a great deal higher.
Fitting this type of model does not constrain measurement error to be transmitted phenotypically and thus is likely to provide more realistic parameter estimates than a casual model without residual error terms.
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Advanced solutions to these models allows for more realistic parameters to be considered.
An alternative approach is used to evaluate net power output and cycle thermal efficiency from more realistic parameters such as air fuel ratio, fuel mass flow rate, intake temperature, engine design parameters, etc.
The results serve to demonstrate the usefulness of these for constructing instantaneous maps and illustrating morphology of ionospheric storms and provide users with more realistic parameters for radio communications.
The issue becomes much more complex, however, as the theory's simplifying assumptions a single factor of production, a given stock of resources, full employment, and a balanced exchange of goods—are replaced by more-realistic parameters.
The geomagnetic field-line-integrated ionospheric conductivity model used to calculate the ionospheric conductivities in Eq. 4 will be briefly discussed in the next section since it has recently been updated to include more realistic atmospheric parameters.
However, at more realistic model parameters, e.g., a smaller Ekman number, it seems likely that these models remain applicable only when a much stronger forcing is applied to sufficiently break the typical z-invariance of the flow (geostrophy).
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more realistic criterion
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more realistic variables
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more free parameter
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more stable parameter
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