The phrase "artificial distribution" is correct and usable in written English.
It can be used in contexts related to statistics, economics, or data science, where a distribution is generated or manipulated through artificial means or algorithms.
Example: "The researchers employed an artificial distribution to simulate the data for their analysis, ensuring a controlled environment for testing their hypotheses."
Alternatives: "synthetic distribution" or "simulated distribution".
In addition, even with a sharp choice for the artificial distributions γ i, 1≤i≤n, FFBS-based methods outperform two-filter-based smoothers for this model.
Even when measurement times may be assumed to be concentrated on single time points, our method can be used as a kind of regularization of the standard particle filter method if artificial distributions with highly concentrated masses around the measurement points are introduced.
Ordered Ge-island chains on Si(0 0 1) show that artificial strain distribution design is a powerful tool for nanostructure integration.
They have been defined mathematically in the paper by designing a bottom-up agent model which emerges the artificial tree distribution by mediating to the simulation.
The objective is to have the AMR navigate to a target location by: (i) producing an RSS-based artificial magnitude distribution in the navigation region, (ii) using particle filtering based bearing estimation for orientation information, and (iii) using interpolated pseudogradient for efficient path planning and navigation.
However, we choose to keep the initial SEGM as it includes the shape of the topography, which would be absent if simulated by some artificial mass distribution.
As a second input for our nanofocus scattering simulations, we use a beam spot profile which, on the one hand, can be set to any artificial intensity distribution for the desired spot shape.
In this study, for the regions in which microzonation study was not conducted, geological units, engineering surface geology, alluvial layer thickness, tertiary layer thickness, and wide-scaled artificial fill distribution information were evaluated in order to assign a V s30 value for each specified grid.
In order to assess the resolving power of the inversion scheme described in the previous section, before inverting the actual dataset we perform a checkerboard resolution test using synthetic data calculated from an artificial slip distribution (i.e., a "checkerboard" pattern).
