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The second step consists of calculating a random quaternion, q v s j m, inside the spatial range described by the six extremity quaternions, q v s j m i, (calculated in Equation (2)), as follows: q v ′ s j = q ̄ v ̄ s j ± max i q ̄ v ̄ s j - q v s j i * rand[0,1] q v s j = q v ′ s j q v ′ s j, (3).
The mean intensity M i calculated by M i = ∑ j = 1 n S ij n The standard deviation σ i calculated by σ i = S ij − M i 2 n − 1, The coefficient of variation CV i calculated by C V i = σ i M i Where j=1 to n, n represents the number of samples in a population, S ij represents the expression signal of gene i in sample j.
Similar(58)
The magnitude M i is calculated at each station using the equation: where A v is the maximum amplitude in cm/s and r is an epi-central distance in km (Watanabe, 1971).
The slopes of the dose-response functions, or m i, were calculated using ordinary least squares regression.
Over all environments, an adjusted entry mean M i was calculated for each of the 205 clones as: M i = μ ∧ + g ∧ i, where μ ∧ and g ∧ i denote the generalized least square estimates of μ and g i, respectively.
m i is the mass of contaminant removed [kg] during year i calculated as: m i = ∑ j = 1 N we l i Q ij c ¯ ij × β (17).
InSAR data include the effects of both the M j 6.5 and M j 6.4 events, and thus, I calculated a seismically estimated focal mechanism combining both the events, using moment tensor components determined by JMA (2016b) [Fig. 3a(1)].
We compute the time trajectories for all m i then calculate heteroplasmy by setting M1 = m1 + m3, M2 = m2 + m4, respectively the total numbers of wildtype and mutant mtDNAs, and using Equations 15, 16, where all means and variances are straightforwardly extracted from the above analysis.
I calculated Kandi's M-Score based on annual accounts from 2010 to 2012, and on quarterly accounts for the last three quarters.
For a service s v in I i where I i is the set of services that have usage information within pattern M i we calculate the similarity of s j and s v.
The obtained codestream has been decompressed using Kakadu 6.0, and M i has been calculated as the distortion of the reconstructed frame.
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Since I tried Ludwig back in 2017, I have been constantly using it in both editing and translation. Ever since, I suggest it to my translators at ProSciEditing.

Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com