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The cantilever width, b, is the dominant length scale of the flow [13].
For all modes of change, the dominant length scale was dictated by the breakwater dimensions and locations.
It was found that the dominant length scale effects are those that coincide with the direction of fracture, as defined by the orientation of a pre-existing crack.
Furthermore, the continuum hypothesis is valid because the mean-free-path of the molecules in liquid is very small compared to the dominant length b and the gap size g, i.e., Knudsen numbers « 1 [15].
Overall, concordance was high between dominant length variant calls in these regions.
More interestingly, 24 nt is the dominant length for both the sRNAs and the miRNAs highly accumulated in the root tips.
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The algorithm captures low frequency non-dominant length variants, specified by a tunable threshold.
It is observed that shrinkage is dominant along length and width direction of built part.
On the other hand, there are processes with a dominant microscopic length scale, such as small Nernst diffusion thickness in heat/mass transfer [13], small hydraulic radius in microfluidics [14 17], small pore diameter in filtration [5], etc., where the bulk rheology characteristics should be completed using another kind of information.
An assumption that the AGWs caused by the eruption resulted in the small-scale FACs gives a consistent explanation for the MRs. The latitudinal extension of the wave packet, i.e., the scale of ionospheric E-layer dynamo region is about 1700 km, and the dominant wave length is about 180 km.
An assumption that the AGWs caused by the eruption resulted in the small-scale FACs gives a consistent explanation for the MRs. The latitudinal extension of the wave packet, i.e., the scale of ionospheric E-layer dynamo region is about 1700 km, and the dominant wave length is about 180 km. 2.
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Justyna Jupowicz-Kozak
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