in two or more variables

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1: 18.37 Classical OP’s in Two or More Variables
§18.37 Classical OP’s in Two or More Variables
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2: Mark J. Ablowitz
… ►Some of the relationships between IST and Painlevé equations are discussed in two books: Solitons and the Inverse Scattering Transform and Solitons, Nonlinear Evolution Equations and Inverse Scattering. …
3: Bibliography Y
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  • Z. M. Yan (1992) Generalized Hypergeometric Functions and Laguerre Polynomials in Two Variables. In Hypergeometric Functions on Domains of Positivity, Jack Polynomials, and Applications (Tampa, FL, 1991), Contemporary Mathematics, Vol. 138, pp. 239–259.
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    4: 1.5 Calculus of Two or More Variables
    §1.5 Calculus of Two or More Variables
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    5: 8.13 Zeros
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  • (a)

    two zeros in each of the intervals − 2 ⁢ n < a < 2 − 2 ⁢ n when x < 0 ;

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  • (b)

    two zeros in each of the intervals − 2 ⁢ n < a < 1 − 2 ⁢ n when 0 < x ≤ x n ∗ ;

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    6: 28.33 Physical Applications
    … ►Mathieu functions occur in practical applications in two main categories: ►
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    Boundary-values problems arising from solution of the two-dimensional wave equation in elliptical coordinates. This yields a pair of equations of the form (28.2.1) and (28.20.1), and the appropriate solution of (28.2.1) is usually a periodic solution of integer order. See §28.33(ii).

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    7: Sidebar 21.SB1: Periodic Surface Waves
    … ►Two-dimensional periodic waves in a shallow water wave tank. Taken from Joe Hammack, Daryl McCallister, Norman Scheffner and Harvey Segur, “Two-dimensional periodic waves in shallow water. …The caption reads “Mosaic of two overhead photographs, showing surface patterns of waves in shallow water”. …
    8: 19.27 Asymptotic Approximations and Expansions
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    19.27.7 R D ⁡ ( x , y , z ) = 3 2 ⁢ z 3 / 2 ⁢ ( ln ⁡ ( 8 ⁢ z a + g ) − 2 ) ⁢ ( 1 + O ⁡ ( a z ) ) , a / z → 0 .
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    19.27.8 R D ⁡ ( x , y , z ) = 3 x ⁢ y ⁢ z − 6 x ⁢ y ⁢ R G ⁡ ( x , y , 0 ) ⁢ ( 1 + O ⁡ ( z g ) ) , z / g → 0 .
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    19.27.9 R D ⁡ ( x , y , z ) = 3 x ⁢ z ⁢ ( y + z ) ⁢ ( 1 + O ⁡ ( b x ⁢ ln ⁡ x b ) ) , b / x → 0 .
    … ►The approximations in §§19.27(i)–19.27(v) are furnished with upper and lower bounds by Carlson and Gustafson (1994), sometimes with two or three approximations of differing accuracies. … ►A similar (but more general) situation prevails for R − a ⁡ ( 𝐛 ; 𝐳 ) when some of the variables z 1 , … , z n are smaller in magnitude than the rest; see Carlson (1985, (4.16)–(4.19) and (2.26)–(2.29)). …
    9: 19.20 Special Cases
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    19.20.19 R D ⁡ ( x , y , z ) ∼ 3 ⁢ x − 1 / 2 ⁢ y − 1 / 2 ⁢ z − 1 / 2 , z / x ⁢ y → 0 .
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    19.20.20 R D ⁡ ( x , y , y ) = 3 2 ⁢ ( y − x ) ⁢ ( R C ⁡ ( x , y ) − x y ) , x ≠ y , y ≠ 0 ,
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    19.20.21 R D ⁡ ( x , x , z ) = 3 z − x ⁢ ( R C ⁡ ( z , x ) − 1 z ) , x ≠ z , x ⁢ z ≠ 0 .
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    19.20.22 ∫ 0 1 t 2 ⁢ d t 1 − t 4 = 1 3 ⁢ R D ⁡ ( 0 , 2 , 1 ) = ( Γ ⁡ ( 3 4 ) ) 2 ( 2 ⁢ π ) 1 / 2 = 0.59907 01173 67796 10371 ⁢ … .
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    19.20.23 R D ⁡ ( x , y , a ) = R − 3 4 ⁡ ( 5 4 , 1 2 ; a 2 , x ⁢ y ) , a = 1 2 ⁢ x + 1 2 ⁢ y .
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    10: 18.40 Methods of Computation
    … ►In what follows this is accomplished in two ways: i) via the Lagrange interpolation of §3.3(i) ; and ii) by constructing a pointwise continued fraction, or PWCF, as follows: …