For fluid turbulence, V is associated with the root-mean-square of the large-scale velocity fluctuation.
For stations in eastern Taiwan (e.g., stations TWD, HWA, EGFH), complex structures, including the detailed plate boundary of the Longitudinal Valley and Ryukyu subduction zone, were not well explained by the large-scale velocity model used (Huang et al., 2014).
Wavelet transform was used to separate small scale fluctuations from large scale fluctuations in liquid velocity field.
When 31 thin internals are inserted in column at a low superficial gas velocity, large scale liquid circulations are replaced by small local vortex.
It has been noticed that a large scale impulsion of cross-velocity exists in the gap region, which plays an important role on the transverse mixing flow and heat transfer.
Further to the West, at the western arc of the Alps there is a good correlation (at large scale) between anisotropy, the high-velocity zones (tomographic images), Bouguer gravity anomalies, and the topographic feature of the mountains.
The maximum velocity of anti-sunward flow is ~2800 m/s, which is much faster than the large-scale background velocity of ~500 m/s that can be seen toward the end of this time interval.
The metastable zone (MSZ) of MgCl2·6H2O·1,4-dioxane in the MgCl2-6H2O-1,4-dioxane system was studied using an IR probe in small scale (12 mL) and an ultrasound velocity probe in large scale (120 mL).
However, the variations of liquid circulations are different at a high superficial gas velocity, when the large scale liquid circulations are always present in the column regardless of inserting 31 thin internals or 8 thick internals.
With all of this potentially large scale lethality floating around, the muzzle velocity of the MCX and other similar assault-type rifles is particularly important.
