Това са думите examples, свързани с advection. Щракнете върху която и да е дума, за да отидете на страницата с подробности за думата. Или, отидете на дефиницията на advection.
This movement can be viewed as the advection of fluid across a coordinate surface.
In oceanography, advection often refers to the horizontal transport of the heat, humidity or salinity of the ocean.
In this model, moisture transport is accomplished through advection.
A light breeze favours advection fog more than a stiff breeze.
The important feature which leads to chaotic advection is the breaking of heteroclinic orbits.
From left to right the bracketed groups of terms represent advection, production, diffusion and dissipation of turbulence energy.
Towards the end, the book gives a short but instructive introduction to the numerical simulation of turbulent diffusion and advection in the sea.
The ratio of the advection cooling to the local cooling decreases with increasing radii.
The advection-diffusion equation (2.8) for the mean concentration of a passive tracer is remarkable in several respects.
Constructing a multi-dimensional oscillation preventing scheme for the advection equation by a rational function.
The fundamental physical idea is that of a balance of vorticity brought into the jet by advection and diffused by friction.
Another desirable property of an advection scheme is the synchronous transport of fluid and tracers.
In this equation the nonlinear terms on the left side represent an advection of the quantity u with advective velocity (u, v, w).
This formulation facilitates the usage of (nearly) nonoscillatory advection schemes for solving these equations numerically.
After the numerical advection step based on (4.2) and (4.3), we need to review the segment structure.
At the outer edges of the plume, however, the production and destruction terms rapidly approach zero and advection and transport balance each other.
However, in interpreting the results of chaotic advection, it must be recognized that solutes diffuse and solid particles move relative to the fluid locally.
Corresponding transverse variation is induced in the downstream periphery; however, it displays significantly greater axial advection due to the greater flow speed there.
In this paper we investigate the spectral and evolutionary properties of relatively simple, linear, advection-diffusion equations.
