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Non linear problems with Fractional Diffusions

Non linear problems with Fractional Diffusions. Luis A. Caffarelli The University of Texas at Austin. Non linear problems involving fractional diffusions appear in several areas of applied mathematics: Boundary diffusion (see for instance Duvaut and Lions)

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Non linear problems with Fractional Diffusions

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  1. Non linear problems with Fractional Diffusions Luis A. Caffarelli The University of Texas at Austin

  2. Non linear problems involving fractional diffusions • appear in several areas of applied mathematics: • Boundary diffusion (see for instance Duvaut and Lions) • or more generally calculus of variations when the energy • integrals involved correspond to fractional derivatives. • Fluid dynamics like in the quasi-geostrophic equation • modeling ocean atmospheric interaction, or in the case of • turbulent transport • Stochastic processesof discontinuous nature (Levy processes) in • applications for which random walks have jumps at many • different scales (Stocks, insurance)

  3. Remark: the work just described is strongly based in an extension theorem: It identifies the fractional Laplacian of a given function u(x) in Rnwith the normal derivative of an extension v(x,y) of u(x) into the upper half space, (y>0), of Rn+1.

  4. The classical example is the ½ Laplacian: If v is the harmonic extension of u ( convolution with the Poison kernel), then the normal derivative of v at y=0 is exactly the half Laplacian of u.

  5. In particular, u being “half harmonic” simply means that v is harmonic across y=0, reducing regularity properties of u to those of the harmonic function v

  6. In fact, any other fractional power of the Laplacian of a given function u(x) can be realized as the normal derivative of an appropriate extension v(x,y). This can be interpreted as an extension into a space of “fractional dimension” and suggest the correct form of homogeneous solutions, monotonicity formulas, truncated test functions, etc

  7. This “harmonic” extension has the virtue of reducing many global issues and arguments to local, more familiar methods of the calculus of variations. The global properties of the solutions are somehow encoded in the restriction of the extension v(x,y) to unit ball in one more dimension.(L.C and L.Silvestre, arXiv.org, 07)

  8. i) The quasi-geostrophic equation

  9. See also:Kiselev, Nasarov, Volberg, arXiv.org’06

  10. ii) Problems with constrains or Free Boundary problems

  11. iv) Random Homogenization

  12. See the work of D. Cioranescu and F. Murat (1982) where the Homogenized equation was derived for periodic media.

  13. Fully non-linear equations with fractional diffusion

  14. . . .

  15. . Formally, the solution u0to a fully non-linear equation, its first derivatives and its second derivatives all satisfy equations or inequalities like (1) above. This implies that u0 is classical (Evans – Krylov)

  16. Thank you for your attention

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