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Here we have shown that this type of replication where effects are significant but in different directions can be explained by allele frequency differences and gene-gene interactions.
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The spreading of the backwash direction can be explained by the combination of the local topography and temporal evolution of water velocity and flow depth.
The observed change of OCP in the electropositive direction can be explained by an increase in the rate of the cathodic reaction.
The variation of ratcheting life with different angle to rolling direction can be explained by the alteration of yield stress to ultimate tensile strength ratio with the angle to rolling direction.
The characteristics of the near-tip strain fields suggest that the experimental observations of shallow surface cracks (Case A cracks) propagating in the maximum shear strain direction can be explained by a fracture mechanics crack growth criterion based on the maximum effective strain of the near-tip fields for small cracks under general yielding conditions.
The difference in FWHM between the x- and the y-direction can be explained by an azimuthally inhomogeneous intensity distribution around the central STED beam minimum.
Most of the variation in this measure is random, only 21% (horizontal x-direction) and 16% (vertical y-direction) can be explained by individual differences, while the effect sizes of the eye and task are negligible.
Here we provide experimental evidence that the direction of guidance can be explained by the stochastic fluctuations of UNC-40 asymmetric outgrowth activity.
Together these results indicate that the direction and timing of UNC-6 guidance can be explained by the stochastic fluctuation of intracellular UNC-40 outgrowth activity and the exertion of a bias by multiple cues.
Most of the breakouts show directions that can be explained by the regional convergence, but some are obviously rotated by faults and fractures in the megasplay fault zone and in its hanging wall.
The focal mechanisms of local earthquakes also indicate complex tectonic stress regimes in the study area and suggest that the extensional stress field occurs not only in the arc-perpendicular direction but also in the arc-parallel direction, which can be explained by the outward migration of the arc (Kubo and Fukuyama 2003).
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com