(a) Results of reconstruction by the method which fixes the parameters β s, t ( i ) = 1, (b) results of reconstruction by the method which fixes the parameters β s, t ( i ) = 2, (c) zoomed portion of (a), (d) zoomed portion of (b), (e) zoomed portion of the proposed method (Zoomed portion of Figure 2c), (f) a map of the estimated parameters β s, t ( i ) for obtaining Figure 2c in our method.
However, the current simulation method, which fixes the server heat generation and the supply and return air temperature difference of the computer room air handler (CRAH), does not correctly reflect current cooling systems.
The observed number of alleles in a sample is highly dependent on sample size, therefore allelic richness and private allelic richness was calculated using HP-Rare 1.1 [15] correcting for sample size (n) in each region using the rarefaction method, which fixes n as the smallest number of individuals typed for a locus in a sample [16].
Since our data demonstrate that NEUROD2 binding was not exclusive to promoter regions or TSS-proximal sequences, we decided to employ a method for assigning individual peaks to genes which would also account for TSS-distant peaks, as opposed to methods which set fixed windows around TSSs for peak capturing.
As the particle number concentration can be very different in different regions of the simulated reactor volume, we introduce here also a weighting method which allows fixing the number of simulation particles per cell.
The distance-dependent reaction probability derived from the Fokker-Planck Equation as outlined above based on Equations (12) and (13) (cf. [ 51, 52]) requires a look-up table and is therefor slower than a method which uses a fixed critical reaction radius (and if necessary a fixed reaction probability).
Data from qPCR analyses have commonly been evaluated using a fit point method, which uses a fixed threshold based on the difference in baseline fluorescence intensities to determine the Cq value of each sample.
We demonstrate these new CB methods achieve better ensemble decision accuracy than methods which apply fixed rules in combining classifier decisions.
Here we introduce a new method in which we included the varying shell heights derived from the ionosonde to map the slant total electron content from GPS to obtain a more precise vertical total electron content of the ionosphere contrary to some previous methods which used fixed shell heights.
Nevertheless, the MSD values observed for the association mapping methods, which include fixed effects such as the Q 1 K T o p t, Q 2 K T o p t, or PK T o p t, were lower than that of the K T o p t. Therefore, in our study the Q 1 K T o p t, Q 2 K T o p t or PK T o p t are the most appropriate methods for association mapping.
In this study, a mixed geographically weighted regression (MGWR) method which can deal with fixed and varying spatial relationships between a target variable and its environmental variables were proposed and used to predict topsoil soil organic matter (SOM) concentration in two study areas (Heshan, Heilongjiang province and Xuancheng, Anhui province, China) at two scales.
