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1: 13.28 Physical Applications
§13.28(i) Exact Solutions of the Wave Equation
The reduced wave equation 2 w = k 2 w in paraboloidal coordinates, x = 2 ξ η cos ϕ , y = 2 ξ η sin ϕ , z = ξ η , can be solved via separation of variables w = f 1 ( ξ ) f 2 ( η ) e i p ϕ , where …
2: 28.32 Mathematical Applications
§28.32(i) Elliptical Coordinates and an Integral Relationship
If the boundary conditions in a physical problem relate to the perimeter of an ellipse, then elliptical coordinates are convenient. …
§28.32(ii) Paraboloidal Coordinates
The general paraboloidal coordinate system is linked with Cartesian coordinates via …
3: 12.17 Physical Applications
§12.17 Physical Applications
in Cartesian coordinates x , y , z of three-dimensional space (§1.5(ii)). By using instead coordinates of the parabolic cylinder ξ , η , ζ , defined by … In a similar manner coordinates of the paraboloid of revolution transform the Helmholtz equation into equations related to the differential equations considered in this chapter. … …
4: 28.31 Equations of Whittaker–Hill and Ince
§28.31(iii) Paraboloidal Wave Functions
With (28.31.10) and (28.31.11), …are called paraboloidal wave functions. … More important are the double orthogonality relations for p 1 p 2 or m 1 m 2 or both, given by …
Asymptotic Behavior
5: Bibliography U
  • K. M. Urwin (1964) Integral equations for paraboloidal wave functions. I. Quart. J. Math. Oxford Ser. (2) 15, pp. 309–315.
  • K. M. Urwin (1965) Integral equations for the paraboloidal wave functions. II. Quart. J. Math. Oxford Ser. (2) 16, pp. 257–262.
  • 6: 36.5 Stokes Sets
    For z 0 , the Stokes set is expressed in terms of scaled coordinates
    36.5.7 X = 9 20 + 20 u 4 Y 2 20 u 2 + 6 u 2 sign ( z ) ,
    36.5.10 160 u 6 + 40 u 4 = Y 2 .
    With coordinates
    36.5.17 Y S ( X ) = Y ( u , | X | ) ,
    7: 20 Theta Functions
    Chapter 20 Theta Functions
    8: 29.18 Mathematical Applications
    §29.18(i) Sphero-Conal Coordinates
    when transformed to sphero-conal coordinates r , β , γ : …
    29.18.4 u ( r , β , γ ) = u 1 ( r ) u 2 ( β ) u 3 ( γ ) ,
    §29.18(ii) Ellipsoidal Coordinates
    The wave equation (29.18.1), when transformed to ellipsoidal coordinates α , β , γ : …
    9: Bibliography
  • M. J. Ablowitz and H. Segur (1977) Exact linearization of a Painlevé transcendent. Phys. Rev. Lett. 38 (20), pp. 1103–1106.
  • A. Adelberg (1992) On the degrees of irreducible factors of higher order Bernoulli polynomials. Acta Arith. 62 (4), pp. 329–342.
  • S. V. Aksenov, M. A. Savageau, U. D. Jentschura, J. Becher, G. Soff, and P. J. Mohr (2003) Application of the combined nonlinear-condensation transformation to problems in statistical analysis and theoretical physics. Comput. Phys. Comm. 150 (1), pp. 1–20.
  • D. E. Amos (1989) Repeated integrals and derivatives of K Bessel functions. SIAM J. Math. Anal. 20 (1), pp. 169–175.
  • F. M. Arscott (1967) The Whittaker-Hill equation and the wave equation in paraboloidal co-ordinates. Proc. Roy. Soc. Edinburgh Sect. A 67, pp. 265–276.
  • 10: 26.2 Basic Definitions
    A k-dimensional lattice path is a directed path composed of segments that connect vertices in { 0 , 1 , 2 , } k so that each segment increases one coordinate by exactly one unit. …
    Table 26.2.1: Partitions p ( n ) .
    n p ( n ) n p ( n ) n p ( n )
    3 3 20 627 37 21637