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with imaginary periods

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21: 21.2 Definitions
With z 1 = x 1 + i y 1 , z 2 = x 2 + i y 2 ,
21.2.4 θ ^ ( x 1 + i y 1 , x 2 + i y 2 | [ i 1 2 1 2 i ] ) = n 1 = n 2 = e π ( n 1 + y 1 ) 2 π ( n 2 + y 2 ) 2 e π i ( 2 n 1 x 1 + 2 n 2 x 2 n 1 n 2 ) .
21.2.7 θ [ 𝟎 𝟎 ] ( 𝐳 | 𝛀 ) = θ ( 𝐳 | 𝛀 ) .
Characteristics whose elements are either 0 or 1 2 are called half-period characteristics. For given 𝛀 , there are 2 2 g g -dimensional Riemann theta functions with half-period characteristics. …
22: 31.2 Differential Equations
§31.2(iv) Doubly-Periodic Forms
Jacobi’s Elliptic Form
Weierstrass’s Form
ζ = i K + ξ ( e 1 e 3 ) 1 / 2 ,
where 2 ω 1 and 2 ω 3 with ( ω 3 / ω 1 ) > 0 are generators of the lattice 𝕃 for ( z | 𝕃 ) . …
23: 1.18 Linear Second Order Differential Operators and Eigenfunction Expansions
Case 3: Periodic Boundary Conditions: ϕ ( 0 ) = ϕ ( π ) and ϕ ( 0 ) = ϕ ( π ) . … More generally, continuous spectra may occur in sets of disjoint finite intervals [ λ a , λ b ] ( 0 , ) , often called bands, when q ( x ) is periodic, see Ashcroft and Mermin (1976, Ch 8) and Kittel (1996, Ch 7). … Then dim N z is constant for z > 0 and also constant for z < 0 . Put n + = dim N z ( z > 0 ) and n = dim N z ( z < 0 ), the deficiency indices for T . …Then any self-adjoint extension of T is determined by a linear isometry U : N i N i and it is the restriction of T to { v + w + U w v 𝒟 ( T ) , w N i } . …
24: 23.2 Definitions and Periodic Properties
§23.2 Definitions and Periodic Properties
§23.2(iii) Periodicity
Hence ( z ) is an elliptic function, that is, ( z ) is meromorphic and periodic on a lattice; equivalently, ( z ) is meromorphic and has two periods whose ratio is not real. … The function ζ ( z ) is quasi-periodic: for j = 1 , 2 , 3 , … For further quasi-periodic properties of the σ -function see Lawden (1989, §6.2).
25: 2.10 Sums and Sequences
As in §24.2, let B n and B n ( x ) denote the n th Bernoulli number and polynomial, respectively, and B ~ n ( x ) the n th Bernoulli periodic function B n ( x x ) . … From §24.12(i), (24.2.2), and (24.4.27), B ~ 2 m ( x ) B 2 m is of constant sign ( 1 ) m . … where α and β are real constants with e i β 1 . … where 𝒞 comprises the two semicircles and two parts of the imaginary axis depicted in Figure 2.10.1. … Here the branch of ( e i α z ) 1 / 2 is continuous in the z -plane cut along the outward-drawn ray through z = e i α and equals e i α / 2 at z = 0 . …
26: 1.8 Fourier Series
Formally, if f ( x ) is a real- or complex-valued 2 π -periodic function, … If f ( x ) is of period 2 π , and f ( m ) ( x ) is piecewise continuous, then … If f ( x ) and g ( x ) are continuous, have the same period and same Fourier coefficients, then f ( x ) = g ( x ) for all x . … Let f ( x ) be an absolutely integrable function of period 2 π , and continuous except at a finite number of points in any bounded interval. … If a function f ( x ) C 2 [ 0 , 2 π ] is periodic, with period 2 π , then the series obtained by differentiating the Fourier series for f ( x ) term by term converges at every point to f ( x ) . …
27: 23.7 Quarter Periods
§23.7 Quarter Periods
23.7.2 ( 1 2 ω 2 ) = e 2 i ( e 1 e 2 ) ( e 2 e 3 ) = e 2 i ω 1 2 ( K ( k ) ) 2 k k ,
28: 1.15 Summability Methods
If f ( θ ) is periodic and integrable on [ 0 , 2 π ] , then as n the Abel means A ( r , θ ) and the (C,1) means σ n ( θ ) converge to …
1.15.25 n = F ( n ) e i n θ
The imaginary part
1.15.40 Φ ( x + i y ) = 1 π f ( t ) x t ( x t ) 2 + y 2 d t
Moreover, lim y 0 + Φ ( x + i y ) is the Hilbert transform of f ( x ) 1.14(v)). …
29: 21.9 Integrable Equations
21.9.2 i u t = 1 2 u x x ± | u | 2 u .
The KP equation has a class of quasi-periodic solutions described by Riemann theta functions, given by …
See accompanying text
Figure 21.9.1: Two-dimensional periodic waves in a shallow water wave tank, taken from Hammack et al. (1995, p. 97) by permission of Cambridge University Press. … Magnify
30: 3.5 Quadrature
If in addition f is periodic, f C k ( ) , and the integral is taken over a period, then …
3.5.37 c i c + i e ζ ζ s p k ( 1 / ζ ) p ( 1 / ζ ) d ζ = 0 , k ,
3.5.39 g ( t ) = 1 2 π i σ i σ + i e t p G ( p ) d p ,
The steepest descent path is given by ( t 2 t ) = 0 , or in polar coordinates t = r e i θ we have r = sec 2 ( 1 2 θ ) . …The integrand can be extended as a periodic C function on with period 2 π and as noted in §3.5(i), the trapezoidal rule is exceptionally efficient in this case. …