Multi-scale expansions in the theory of systems integrable by the inverse scattering transform
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Citations
Wave collapse in physics: principles and applications to light and plasma waves
Dark solitons in atomic Bose–Einstein condensates: from theory to experiments
Dark solitons in atomic Bose-Einstein condensates: from theory to experiments
Nonlinear waves in Bose-Einstein condensates: physical relevance and mathematical techniques
The Mechanism for Frequency Downshift in Nonlinear Wave Evolution
References
Linear and Nonlinear Waves
Linear and Nonlinear Waves
Multiphase averaging and the inverse spectral solution of the Korteweg—de Vries equation
Related Papers (5)
Frequently Asked Questions (9)
Q2. What is the common name for the multiscale expansion method?
application of multi-scale expansions to the integrable systems in most cases leads to one of the classical equations which at one time made famous the inverse scattering transform-the nonlinear Schrtidinger equation (NSE), the Korteweg-deVries equation (KdV), the DaveyStewartson equation (DS), the system of N-waves.
Q3. What is the simplest way to describe a quasi-monochromatic wave?
For potentials in the form of a quasimonochromatic wave (2.2) the reflection coefficient in these points has sharp peaks corresponding to the strong resonance subbarrier reflection.
Q4. What is the purpose of the results?
The authors suppose that these results will be useful for further development of the theory of fundamental two-dimensional s y s t e m s - K P and DS equations, the twodimensional N-wave problem-which from their point of view, is far from being completed.
Q5. how do the authors find the first order terms in e?
from the requirement of vanishing the terms of zero order in e the authors find q = 2p 3. Simultaneously in (2.10) the first order terms are cancelled.
Q6. What is the common way to solve a nonlinear wave problem?
if it is already known that the solution represents a set of one or more quasimonochromatic wave packets of a small amplitude, it is reasonable to turn to a set of equations for complex envelopes of these packets.
Q7. what is the k = lu 1 -- e 2 u?
(5.5) k = lU 1 ~-- e 2 U ( X ,, i t ) , Z t = ex, t ' = e3t,u 2 = 1, ~ + ~ ( ~ ' ) , ¢1~ = ' :e i°¢(x ', t'),0 = k x - 2 k 3 t - 3 i e 2 k [ t k ( t ) d t . j - -(4.10)By substituting (4.10) into (3.1) the authors have as e ~ 0Ou 03U + 3 ~ x ( U 2 + Iq~[ 2) 0, 0--7 + Ox 3 -x ( t )¢+¢xx+ u¢=0. (4.11)Hereoov= E ~2kVk(x', t'), k = lx ' = e ( x - - l ) , t ' = e 3 t .
Q8. what is the l-operator for the nonlinear Schrtlinger?
In particular, the authors haveV 1 O - 1 • 3 = VI01 0_ 3 = (2.14) 2k 2 , 2k 2At n = + l w e f i n di 001 --ff~xt --[-~O_1 =/.LO1,. 0 0 _ 1 - - l ~ q - l ~ * O l ~ - - - / . L O _ 1.(2.15)In the system (2.15) the authors find out the L-operator forthe nonlinear Schrt~linger equation (2.8).
Q9. How can the authors simplify the wave dispersion law?
on the contrary, the authors are interested in extremely long-wave weak nonlinear oscillations, the problem can be simplified by expanding the wave dispersion law in the neighbourhood of the wave number k equal to zero, then by passing to the moving coordinate system the authors can eliminate the terms linear with respect to a wave number- the KdV equation is usually derived in this way.