Instead of the make-believe sets or an anywhere emptiness, many stores have introduced large-scale background photographs of models wearing garments and accessories, a few of which are actually placed in the window's foreground.
Particularly, in the hybrid system, the solver for incompressible flow on overset meshes (SIFOM) resolves fully 3D small-scale local flow phenomena, while the unstructured grid finite volume coastal ocean model (FVCOM) captures large-scale background flows.
While ultrasonic waveform tomography has succeeded in detecting such features, recovery is difficult because it requires computationally expensive high-frequency numerical wave simulations and an accurate understanding of large-scale background variations of the engineered structure.
The regional Pb isotope ratio distributions show that the ratios show little variation for a large central part of the country and provide the large-scale background isotope ratios for the Czech Republic of about 204Pb/206Pb = 0.0550, 206Pb/207Pb = 1.167, 206Pb/208Pb = 0.478 and 207Pb/208Pb = 0.409 for 2010.
Under the large-scale background of lake filling, K1q4 of the Quantou Formation includes three lake drainage sub-cycles and three lake filling sub-cycles.
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.
And according to the scale divisions of low-frequency components, we can determine the specific low-frequency components required for large-scale background of elastic parameters (Cao et al. 2009; Yang and Wu 2016).
The maximum anti-sunward velocity reached ~2800 m/s, and this is almost an order of magnitude larger than the large-scale background flow seen deep in the polar cap later in this time interval (~300 m/s).
Flow velocities over the patches are substantially larger than in the surrounding regions that would represent large-scale background convection, and the flow channel widths are comparable to the enhanced density widths.
In a majority (45) of events, longitudinally narrow flow enhancements directed anti-sunward are found to be collocated with the patches, have velocities (up to a few km/s) substantially larger than the large-scale background flows (~500 m/s) and have widths comparable to patch widths (~400 km).
