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Encyclopedia > Advection equation

The advection equation is the partial differential equation that governs the motion of a conserved scalar as it is advected by a known velocity field. It is derived using the scalar's conservation law, together with Gauss's theorem, and taking the infinitesimal limit. In mathematics, and in particular analysis, a partial differential equation (PDE) is an equation involving partial derivatives of an unknown function. ... The concept of a scalar is used in mathematics, physics, and computing. ... Advection is the transport of a conserved scalar quantity that is transported in a vector field. ... Vector field given by vectors of the form (-y, x) In mathematics a vector field is a construction in vector calculus which associates a vector to every point in a Euclidean space. ... In physics, a conservation law states that a particular measurable property of an isolated physical system does not change as the system evolves. ... In vector calculus, the divergence theorem, also known as Gauss theorem, Ostrogradskys theorem, or Ostrogradsky-Gauss theorem is a result that links the divergence of a vector field to the value of surface integrals of the flow defined by the field. ... In mathematics, an infinitesimal, or infinitely small number, is a number that is greater in absolute value than zero yet smaller than any positive real number. ...


Perhaps the best image to have in mind is the transport of dissolved salt in water.


The advection equation expressed mathematically is:

where ∇· is the divergence. Frequently, it is assumed that the velocity field is solenoidal, that is, that . If this is so, the above equation reduces to In vector calculus, the divergence is an operator that measures a vector fields tendency to originate from or converge upon a given point. ... This article is in need of attention. ...

In particular, if the flow is steady, which shows that ψ is constant along a streamline. You really need to make it way more easier to understand ...


The advection equation is not simple to solve numerically: the system is a hyperbolic partial differential equation, and interest typically centers on discontinuous "shock" solutions (which are notoriously difficult for numerical schemes to handle). Numerical analysis is the study of algorithms for the problems of continuous mathematics (as distinguished from discrete mathematics). ... In mathematics, a continuous function is one in which arbitrarily small changes in the input produce arbitrarily small changes in the output. ...


Even in one space dimension and constant velocity, the system remains difficult to simulate (it is a standard test for advection schemes known as the pigpen problem). The equation becomes

where ψ = ψ(x,t).


According to Zang [2], numerical simulation can be aided by considering the skew symmetric form for the advection operator. In linear algebra, a skew-symmetric (or antisymmetric) matrix is a square matrix A whose transpose is also its negative; that is, it satisfies the equation: AT = −A or in component form, if A = (aij): aij = − aji   for all i and j. ...

where is a vector with components and the notation has been used.


Since skew symmetry implies only complex eigenvalues, this form reduces the "blow up" and "spectral blocking" often experienced in numerical solutions with sharp discontinuities (see Boyd [1] pp. 213). In mathematics, the complex numbers are an extension of the real numbers by the inclusion of the imaginary unit i, satisfying . ... In linear algebra, a scalar λ is called an eigenvalue (in some older texts, a characteristic value) of a linear mapping A if there exists a nonzero vector x such that Ax=λx. ...


References

[1] Boyd, J.P.: 2000, Chebyshev and Fourier Spectral Methods 2nd edition, Dover, New York


[2] Zang, T: 1991, On the rotation and skew-symmetric forms for incompressible flow simulations, Applied Numerical Mathematics,7,27-40.


See also


  Results from FactBites:
 
Advection Summary (624 words)
Although advection processes are important heat equilibration mechanisms for both the atmosphere and the oceans, the speed and volume of mass transported differs greatly between the atmosphere and oceans.
Advection fog usually occurs when the atmosphere is very stable so that moist (humid) air near the surface does not mix vertically with an overlying layer of drier air.
Advection is important for the formation of orographic cloud and the precipitation of water from clouds, as part of the hydrological cycle.
  More results at FactBites »


 
 

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