After marking a trough and two ridges on the 850-hPa map, Cole located an area of CAA, stating, "Cold air
advection you would have down here because you're crossing your wind heights across the temperature lines." He sought additional regions of CAA: "We still have it crossing ...
Equation (4), namely,
advection, can be solved by either a Semi-Lagrangian (Courant et al., 1952) or a first-order upwind scheme.
Warm
advection patterns are nothing to mess around with.
Over East Asia, CNRM-CM5.1 simulated the prevailing wintertime monsoon-related northerly
advection quite well (Figure 6(c)); however, the frequencies of the northwestern and western circulation types were markedly overestimated at the expense of the northeastern circulation type.
For the
advection term, we apply the scheme of either u > 0 or u < 0.
The
advection velocities of the fluid phase and of the solid matrix are denoted as u and w, respectively.
Advection of a large number of markers placed near the interface is tracked to capture an interface.
In stochastic representation, marked particles undergo
advection process by wind at a certain speed and at the same time experience random movement simulating turbulent fluctuation.
The
advection and diffusion terms are substituted by using the centered difference in space by
A ten percent ([+ or -] 10%) change in each parameter (e.g., source concentrations, initial concentrations, vertical velocity, and angle of
advection) yielded only slight percent differences in the final concentrations of lead.
In the present context, the
advection of a turbulent signal from its measurement point [??]AN to a point [[??].sub.c] downwind is schematized in Figure 12.
We now reconsider the local problem examined in Section 2 while allowing for the effect of
advection. It is suggested in [6] and [7] that
advection in a subdiffusive medium can be modeled by adding another fractional derivative term to the basic subdiffusion equation.