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For each radiosonde launch, the weighted mean temperature of the atmosphere T m was computed as (Bevis et al. 1992; Davis et al. 1985) T m = ∫ e / T d h ∫ e / T 2 d h (12).
After subtraction of the DC term and the white noise, the median ω m was computed.
Additional trials were then simulated and the total number of additional participants, m, was computed and recorded.
Then, a vector t of length m was computed such that the entry for the ith marker was ti = 2(pi-0.5), where pi is the minor allele frequency.
A Malthusian growth rate per day (m) was computed according to the expression \documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$m=\frac{1}{tt} \ln {Q}_t $$\end{document} m = 1 t ln Q t.
The expected genetic length of each chromosome (M) was computed as ∑ i = 1 4 i p i where i is the number of crossover events (1/2/3/4) on the corresponding chromosome, and p i is the expected probability of crossover i.
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The detection threshold P T ij m is computed and bcost ij m is initialized to 0. Cost Computation: % Computing bcost.
The initial covariance matrix P m is computed in the same way using multiple rendering pass.
Influences of variation of porosity at a microscopic level on cementation exponent m are computed using the effective-medium theories.
Similar to case 1, the eSVD of H m is computed, and then φ m is calculated.
For each ROI mean values of SUV (= c t ), SUR (= c t / c a ) and K m were computed.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com