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Consequently, the MSF pixel estimates are chi-squared distributed with two degrees of freedom, and such a distribution is a negative exponential Rayleigh distribution [2, 9].
It is also of interest to know how closely packed about its mean value a distribution is.
But averages can be misleading when a distribution is heavily skewed at one end, with a small number of unrepresentative outliers pulling the average in their direction.
Sampling from this, a distribution is very simple.
Solomon proposes a scheme for ascertaining when a distribution is normatively appropriate.
A quantile of a distribution is most commonly termed a 'return level' in flood risk analysis.
Such a distribution is typical of plasma parameters in the geotail lobes.
The traditional way to take draws from a distribution is to use the Pseudo-Monte Carlo approach.
Let us recall that the Fano factor of a distribution is the ratio of its variance over its mean.
A distribution is said to be of Pareto-type if there exists a positive constant such that (1.1).
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The structural significance of this CENP-A distribution is not known, but it may impart directionality onto the centromere structure that is necessary for kinetochore attachment and for bi-directional, anaphase migration of sister chromatids (Allshire and Karpen 2008).
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