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31: 9.13 Generalized Airy Functions
Reid (1972) and Drazin and Reid (1981, Appendix) introduce the following contour integrals in constructing approximate solutions to the Orr–Sommerfeld equation for fluid flow: … Each of the functions A k ( z , p ) and B k ( z , p ) satisfies the differential equation …and the difference equation
32: Errata
  • Equation (18.28.2)
    18.28.2 1 1 p n ( x ) p m ( x ) w ( x ) d x = h n δ n , m , | a | , | b | , | c | , | d | 1 , a b , a c , a d , b c , b d , c d 1

    The constraint of this equation was updated to include a b , a c , a d , b c , b d , c d 1 .

  • Chapter 1 Additions

    The following additions were made in Chapter 1:

  • Additions

    Section: 15.9(v) Complete Elliptic Integrals. Equations: (11.11.9_5), (11.11.13_5), Intermediate equality in (15.4.27) which relates to F ( a , a ; a + 1 ; 1 2 ) , (15.4.34), (19.5.4_1), (19.5.4_2) and (19.5.4_3).

  • Equation (33.14.15)
    33.14.15 0 ϕ m , ( r ) ϕ n , ( r ) d r = δ m , n

    The definite integral, originally written as 0 ϕ n , 2 ( r ) d r = 1 , was clarified and rewritten as an orthogonality relation. This follows from (33.14.14) by combining it with Dunkl (2003, Theorem 2.2).

  • Subsection 19.11(i)

    A sentence and unnumbered equation

    R C ( γ δ , γ ) = 1 δ arctan ( δ sin θ sin ϕ sin ψ α 2 1 α 2 cos θ cos ϕ cos ψ ) ,

    were added which indicate that care must be taken with the multivalued functions in (19.11.5). See (Cayley, 1961, pp. 103-106).

    Suggested by Albert Groenenboom.

  • 33: 28.6 Expansions for Small q
    where k is the unique root of the equation 2 E ( k ) = K ( k ) in the interval ( 0 , 1 ) , and k = 1 k 2 . …
    34: 36.2 Catastrophes and Canonical Integrals
    36.2.28 Ψ ( E ) ( 0 , 0 , z ) = Ψ ( E ) ( 0 , 0 , z ) ¯ = 2 π π z 27 exp ( 2 27 i z 3 ) ( J 1 / 6 ( 2 27 z 3 ) + i J 1 / 6 ( 2 27 z 3 ) ) , z 0 ,
    36.2.29 Ψ ( H ) ( 0 , 0 , z ) = Ψ ( H ) ( 0 , 0 , z ) ¯ = 2 1 / 3 3 exp ( 1 27 i z 3 ) Ψ ( E ) ( 0 , 0 , z 2 2 / 3 ) , < z < .
    35: 25.14 Lerch’s Transcendent
    25.14.5 Φ ( z , s , a ) = 1 Γ ( s ) 0 x s 1 e a x 1 z e x d x , s > 1 , a > 0 if z = 1 ; s > 0 , a > 0 if z [ 1 , ) .
    25.14.6 Φ ( z , s , a ) = 1 2 a s + 0 z x ( a + x ) s d x 2 0 sin ( x ln z s arctan ( x / a ) ) ( a 2 + x 2 ) s / 2 ( e 2 π x 1 ) d x , a > 0 if | z | < 1 ; s > 1 , a > 0 if | z | = 1 .
    36: 29.2 Differential Equations
    This equation has regular singularities at the points 2 p K + ( 2 q + 1 ) i K , where p , q , and K , K are the complete elliptic integrals of the first kind with moduli k , k ( = ( 1 k 2 ) 1 / 2 ) , respectively; see §19.2(ii). …
    37: 22.19 Physical Applications
    22.19.2 sin ( 1 2 θ ( t ) ) = sin ( 1 2 α ) sn ( t + K , sin ( 1 2 α ) ) ,
    Hyperelliptic functions u ( z ) are solutions of the equation z = 0 u ( f ( x ) ) 1 / 2 d x , where f ( x ) is a polynomial of degree higher than 4. …
    38: 32.4 Isomonodromy Problems
    Note that the right-hand side of the last equation is a first integral of the system (32.4.10)–(32.4.13). …
    39: 22.16 Related Functions
    If K x K , then the following four equations are equivalent: …
    22.16.14 ( x , k ) = 0 sn ( x , k ) 1 k 2 t 2 1 t 2 d t ;
    In Equations (22.16.21)–(22.16.23), K < x < K . In Equations (22.16.24)–(22.16.26), 2 K < x < 2 K . …
    40: 6.2 Definitions and Interrelations
    §6.2(i) Exponential and Logarithmic Integrals
    The logarithmic integral is defined by …
    §6.2(ii) Sine and Cosine Integrals