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Turbulent Transfer of Energy by Radiating Pulses Benno Rumpf Physics Institute, Chemnitz University of Technology, 09107 Chemnitz, Germany Alan C. Newell and Vladimir E. Zakharov Department of Mathematics, University of Arizona, Tucson, Arizona 85721, USA (Received 3 June 2009; published 14 August 2009) We propose a new mechanism for turbulent transport in systems which support radiating nonlinear solitary wave packets or pulses. The direct energy cascade is provided by adiabatically evolving pulses, whose widths and carrier wavelengths decrease. The inverse cascade is due to the excitation of radiation. The spectrum is steeper than the Kolmogorov-Zakharov spectrum of wave turbulence. DOI: 10.1103/PhysRevLett.103.074502 PACS numbers: 47.27.E, 47.27.De, 52.35.g, 92.10.c Wave turbulence is a highly successful theory for turbu- lent nonequilibrium processes in plasmas, fluids, and non- linear optics. It provides an analytic connection of the deterministic nonlinear dynamics to statistical properties of a turbulent energy flow [1]. Its description of weakly interacting waves with almost random phases culminates in a kinetic equation for the wave action density. The Kolmogorov-Zakharov (KZ) solutions to this kinetic equa- tion describe the transfer of energy (wave action) from long (short) scales to short (long) scales. The results of Cai and co-workers [2], designed to check wave turbulence theory, threw down the gauntlet for advocates of its uni- versal applicability. They studied a one-dimensional model i _ c ðx; tÞ¼ Lc ðx; tÞþ !c ðx; tÞj c ðx; tÞj 2 ; (1) where c ðx; tÞ is a complex wave amplitude and the linear operator L is defined by L expðikxÞ¼ ! k expðikxÞ with a square-root dispersion ! k ¼ ffiffiffiffiffi jkj p designed to mimic deep water waves. The Majda, McLaughlin, and Tabak (MMT) equation (1) derives from the Hamiltonian E ¼ E 2 þ E 4 , E 2 ¼ R ! k ja k j 2 dk and E 4 ¼ ! R j c j 4 =2dx, with Fourier modes a k ¼ R c ðx; tÞ expðikxÞdx= ffiffiffiffiffiffi 2% p . Conservation of wave action N ¼ R j c j 2 dx and momentum P ¼ i R ð cc x c x c Þdx are related to the phase and transla- tional symmetries of (1). A statistically stationary nonequi- librium state is achieved when external damping is applied at very long scales and at short scales, and driving is applied at long scales. This causes two conserved density cascades, a direct cascade of energy and an inverse cascade of wave action. In wave turbulence both cascades are driven by the same four wave resonances producing long and short waves. The KZ spectrum of the wave action density for the direct cascade is hja k j 2 i k 1 in wave turbulence, which is independent of the sign ! of the nonlinearity. Repeated trials of careful experiments [25] showed that the KZ spectrum is recovered for the MMT equation with ! ¼1. For ! ¼ 1, one finds a steeper spectrum of roughly k 1:25 (Fig. 1). This leads to the following intriguing questions: What new mechanisms are responsible for energy and wave action transfer? What causes the failure of wave turbulence theory? In this Letter, we propose a new mechanism of turbulent transfer that is radically different from that of wave turbu- lence. In repeated simulations of (1), the most striking feature is a spatiotemporal pattern of left- and right- moving localized structures (Fig. 2). Their speeds decrease during their lifetime so that the traces are curved (Fig. 3). We suggest that these evolving coherent wave packets (pulses) cause the cascades of wave action and energy. Their spectral width is initially of the same order as their central wave number so that they have few oscillations and a large central peak (Fig. 4). They resemble giant (freak) waves encountered in the ocean [6] and in optical fibers [7]. These pulses are initiated by a Benjamin-Feir insta- bility, and they arise only in the MMT equation with ! ¼ 1. They emit Cherenkov-like radiation as the solitary ‘‘head’’ resonantly drives long oscillatory ‘‘tails’’ [4,8,9]. The pulse heads change adiabatically, because they lose wave action 0.01 0.1 1 1000 100 10 1 damping inertial range λ=1 λ=−1 N k k damping driving FIG. 1 (color online). Time-averaged power spectra N k ¼ hja k j 2 i for the MMT equation (1). The equation with ! ¼1 yields a Kolmogorov-Zakharov spectrum hja k j 2 i k 1 , and ! ¼ 1 yields a steeper spectrum hja k j 2 i k 1:25 . The system contains L ¼ 4096 nodes, and the wave number space is %<k %. Damping is applied to the modes jkj 10%=L and jkj %=2, and the modes 20%=L < jkj 30%=L are driven externally. PRL 103, 074502 (2009) PHYSICAL REVIEW LETTERS week ending 14 AUGUST 2009 0031-9007= 09=103(7)=074502(4) 074502-1 Ó 2009 The American Physical Society
Transcript
Page 1: Turbulent Transfer of Energy by Radiating Pulsesmath.arizona.edu/~anewell/publications/Turbulent Transfer...This causes the radiation of wave action, energy, and negative momentum

Turbulent Transfer of Energy by Radiating Pulses

Benno Rumpf

Physics Institute, Chemnitz University of Technology, 09107 Chemnitz, Germany

Alan C. Newell and Vladimir E. Zakharov

Department of Mathematics, University of Arizona, Tucson, Arizona 85721, USA(Received 3 June 2009; published 14 August 2009)

We propose a new mechanism for turbulent transport in systems which support radiating nonlinear

solitary wave packets or pulses. The direct energy cascade is provided by adiabatically evolving pulses,

whose widths and carrier wavelengths decrease. The inverse cascade is due to the excitation of radiation.

The spectrum is steeper than the Kolmogorov-Zakharov spectrum of wave turbulence.

DOI: 10.1103/PhysRevLett.103.074502 PACS numbers: 47.27.E�, 47.27.De, 52.35.�g, 92.10.�c

Wave turbulence is a highly successful theory for turbu-lent nonequilibrium processes in plasmas, fluids, and non-linear optics. It provides an analytic connection of thedeterministic nonlinear dynamics to statistical propertiesof a turbulent energy flow [1]. Its description of weaklyinteracting waves with almost random phases culminatesin a kinetic equation for the wave action density. TheKolmogorov-Zakharov (KZ) solutions to this kinetic equa-tion describe the transfer of energy (wave action) fromlong (short) scales to short (long) scales. The results of Caiand co-workers [2], designed to check wave turbulencetheory, threw down the gauntlet for advocates of its uni-versal applicability. They studied a one-dimensional model

i _c ðx; tÞ ¼ Lc ðx; tÞ þ �c ðx; tÞjc ðx; tÞj2; (1)

where c ðx; tÞ is a complex wave amplitude and the linearoperator L is defined by L expðikxÞ ¼ !k expðikxÞ with a

square-root dispersion !k ¼ffiffiffiffiffiffijkjp

designed to mimic deepwater waves. The Majda, McLaughlin, and Tabak (MMT)equation (1) derives from the Hamiltonian E ¼ E2 þ E4,E2 ¼

R!kjakj2dk and E4 ¼ �

R jc j4=2dx, with Fourier

modes ak ¼Rc ðx; tÞ expð�ikxÞdx= ffiffiffiffiffiffiffi

2�p

. Conservation

of wave action N ¼ R jc j2dx and momentum P ¼iRðc c �

x � c xc�Þdx are related to the phase and transla-

tional symmetries of (1). A statistically stationary nonequi-librium state is achieved when external damping is appliedat very long scales and at short scales, and driving isapplied at long scales. This causes two conserved densitycascades, a direct cascade of energy and an inverse cascadeof wave action. In wave turbulence both cascades aredriven by the same four wave resonances producing longand short waves. The KZ spectrum of the wave actiondensity for the direct cascade is hjakj2i � k�1 in waveturbulence, which is independent of the sign � of thenonlinearity. Repeated trials of careful experiments [2–5]showed that the KZ spectrum is recovered for the MMTequation with � ¼ �1. For � ¼ 1, one finds a steeperspectrum of roughly k�1:25 (Fig. 1). This leads to thefollowing intriguing questions: What new mechanisms

are responsible for energy and wave action transfer?What causes the failure of wave turbulence theory?In this Letter, we propose a new mechanism of turbulent

transfer that is radically different from that of wave turbu-lence. In repeated simulations of (1), the most strikingfeature is a spatiotemporal pattern of left- and right-moving localized structures (Fig. 2). Their speeds decreaseduring their lifetime so that the traces are curved (Fig. 3).We suggest that these evolving coherent wave packets(pulses) cause the cascades of wave action and energy.Their spectral width is initially of the same order as theircentral wave number so that they have few oscillations anda large central peak (Fig. 4). They resemble giant (freak)waves encountered in the ocean [6] and in optical fibers[7]. These pulses are initiated by a Benjamin-Feir insta-bility, and they arise only in theMMTequation with � ¼ 1.They emit Cherenkov-like radiation as the solitary ‘‘head’’resonantly drives long oscillatory ‘‘tails’’ [4,8,9]. The pulseheads change adiabatically, because they lose wave action

0.01 0.1 1

1000

100

10

1damping

inertial range

λ=1λ=−1

Nk

k

damping

driving

FIG. 1 (color online). Time-averaged power spectra Nk ¼hjakj2i for the MMT equation (1). The equation with � ¼ �1yields a Kolmogorov-Zakharov spectrum hjakj2i � k�1, and � ¼1 yields a steeper spectrum hjakj2i � k�1:25. The system containsL ¼ 4096 nodes, and the wave number space is ��< k � �.Damping is applied to the modes jkj � 10�=L and jkj � �=2,and the modes 20�=L < jkj � 30�=L are driven externally.

PRL 103, 074502 (2009) P HY S I CA L R EV I EW LE T T E R Sweek ending

14 AUGUST 2009

0031-9007=09=103(7)=074502(4) 074502-1 � 2009 The American Physical Society

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and energy to their resonant radiation tails. We will showthat the direct energy cascade is carried by graduallydeforming pulse heads. The inverse cascade is carried byradiation to the tails. Our simulations make it clear thatpulses interact very little with each other and changeadiabatically. Therefore the field c is dominated by anensemble of noninteracting and evolving pulses whosestatistical properties can be computed as a weighted timeaverage over the history of a single pulse. We can predictthe spectrum by computing the adiabatic change of thewave packet which agrees very closely with what weobserve. This dynamics supercedes four wave resonancesof weak turbulence.

Figure 3 shows the formation of a pulse from an initiallong wave. Such pulses arise from a Benjamin-Feir–typeinstability of a monochromatic wave solution c ¼c 0 expðikmxÞ of (1). Setting c ¼ ðc 0 þ �aÞ expðikmxÞwith �a ¼ �aþ expðiqxÞ þ �a� expð�iqxÞ the frequency

� of �a� is � ¼ �ffiffiffiffiffiffiffiM2

p� ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi

Dð2jc 0j2 þDÞpwith D¼

ð ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffijkmþqjp þ ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffijkm�qjp �2ffiffiffiffiffiffiffiffiffijkmj

p Þ=2, M ¼ ð ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffijkm þ qjp �ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffijkm � qjp Þ=2. For � ¼ 1, � can have an imaginary partcorresponding to an instability. The most unstable sidebandq is at km.

This nonlinear pulse corresponds to an extremum EðfÞ ofthe energy for given values of the momentum PðfÞ and the

wave action NðfÞ. It can be computed with Lagrange multi-pliers from dðE��N � vPÞ ¼ 0. A special case is the

quasisoliton solution c ðsolÞðx; tÞ ¼ qffiffiffiffiffiffiffiffiffiffiffiffi�!00

m

psech½qðx�

!0mtÞ� exp½iðkmx�!mtþ!00

mq2t=2Þ�, which is valid for

almost monochromatic wave packets with q � km and!m ¼ !ðkmÞ [4]. Here !0

m ¼ d!=dkjkm is the group ve-

locity. In contrast to the Benjamin-Feir instability of thenonlinear Schrodinger equation, the wave packet emergingfrom the instability of (1) has q and km of the same order.The pulse contains essentially only one loop, and it can be

written approximately as c ðfÞðx; tÞ ¼ qffiffiffiffiffiffiffi!m

pk�1m fð�Þ

expði�Þ expði�tÞ where f, �, and � are real functionswith @�=@x ¼ q, @�=@t ¼ �qv, @�=@x ¼ km, @�=@t ¼�kmv. The phase frequency in the frame that moves with

the speed v ¼ @EðfÞðNðfÞ; PðfÞÞ=@PðfÞ is � ¼@EðfÞðNðfÞ; PðfÞÞ=@NðfÞ. In Fourier space, (1) is

i _ak �!kak ¼ Tk; (2)

where the nonlinearity Tk for a pulse solution is given by

Tk ¼Z 1

�1c ðfÞjc ðfÞj2 expð�ikxÞdx= ffiffiffiffiffiffiffi

2�p

� q2k�9=4m Fk expð�i�ktÞ; (3)

and Fk is the Fourier transform of f3 expði�Þ. TheDoppler-shifted frequency in (3) is �k ¼ �þ kv. Modesak in (2) are driven by the time-dependent force Tk. Amode with a k value outside the pulse will respond stronglyif it is in resonance!k ¼ �k with the oscillatory frequencyof Tk. The pulse excites the linear wave at k ¼ kres < 0 forkm > 0 (Fig. 4). This causes the radiation of wave action,energy, and negative momentum from the pulse to a longwave. We assume that a pulse emits an amount of wave

action dNðradÞ > 0. Wave action, momentum, and energy ofthe pulse and the radiation are balanced by the conserva-t= 400 1000t=

0

|ψ|0.25 t

x/L

0.250|ψ|2 2

100040000

11 1

0

x/L

x/L

pulse

radiation

FIG. 3 (color online). Time evolution for the initial conditionof c ðx; t ¼ 0Þ ¼ 0:25 expði2�x=LÞ plus weak noise for theMMT equation (� ¼ 1) with no damping and driving. The figureshows traces of regions with high momentum density. A pulseappears by the Benjamin-Feir instability of the initial wave. Itsspeed decays in time as it emits counterpropagating radiation.

0.5x/L0.2−0.2

ψRe

0.2−0.2

0.2

ψIm radiation

pulse

kkmkres 0.15−0.150

50

radiation

pulsek

|a | 2

(b)(a)

FIG. 4 (color online). (a) Pulse and low-amplitude long waveradiation in space. (b) In Fourier space, the pulse has themaximum power at km. The radiation is a narrow peak at kres �ð ffiffiffi

2p � 1Þ2km.

1

200000

x/L

t

FIG. 2 (color online). Pattern of left- and right-moving pulsesin time and space with periodic boundary conditions for theMMT equation with � ¼ 1. The system is damped and driven asin Fig. 1. Pulses appear spontaneously and cross each otherwithout significant loss of power. The speed of the pulses decaysin time.

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074502-2

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tion equations dNðfÞ þ dNðradÞ ¼ 0, dEðfÞ þ dEðradÞ ¼ 0,

dPðfÞ þ dPðradÞ ¼ 0. Multiplying the resonance condition

with the pulse’s decrement of wave action yields ð!res ��� vkresÞdNðfÞ ¼ 0, which is equivalent to the extremumcondition of the pulse dðE��N � vPÞ ¼ 0. In otherwords, the radiating pulse remains an extremum of theenergy with respect to wave action and momentum. We

can obtain a general equation for the relation between PðfÞ

and NðfÞ as follows. Since dEðradÞ ¼ ffiffiffiffiffiffiffiffiffiffijkresjp

dNðradÞ,dPðradÞ ¼ kresdN

ðradÞ, we find ðdEðradÞ=dNðradÞÞ2 ¼�ðdPðradÞ=dNðradÞÞ. From the conservation laws, this trans-lates to

ðdEðfÞðNðfÞ; PðfÞðNðfÞÞÞ=dNðfÞÞ2 ¼ �dPðfÞ=dNðfÞ: (4)

The exact expression EðfÞðNðfÞ; PðfÞÞ is unknown, but thenumerical evidence (Fig. 5) shows that E2 is very much

larger than E4, and that the ratioffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiPðfÞNðfÞp

=EðfÞ is closeto 1. Solving Eq. (4) with the approximated energy func-

tion EðfÞ ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiPðfÞNðfÞp

yields PðfÞ � NðfÞ ffiffi8

p �3 and EðfÞ �NðfÞ ffiffi

2p �1, which is verified by simulations of Fig. 5(b).

This means that the pulse frequency �m ¼ �þ kmvmay be approximated by !m ¼ ffiffiffiffiffiffi

kmp

, and its wave action

NðfÞ by bqk�3=2m with b ¼ R1

�1 f2dx. Its momentum PðfÞ isapproximately kmN

ðfÞ and its energy EðfÞ is approximatelyffiffiffiffiffiffikm

pNðfÞ. The decrements of the share of these quantities

are connected to changes of q > 0 and km > 0 by

dNðfÞ ¼ bk�3=2m ðdq� 3

2qk�1m dkmÞ;

dEðfÞ ¼ bk�1m ðdq� qk�1

m dkmÞ;dPðfÞ ¼ bk�1=2

m ðdq� 12qk

�1m dkmÞ:

(5)

The energy of the radiation at kres is dEðradÞ ¼�

ffiffiffiffiffiffikm

pdNðradÞ, and its momentum is dPðradÞ ¼

��2kmdNðradÞ with � ¼ ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffijkres=kmj

p. The pulse loses wave

action and energy, but gains momentum in this evolution.

Expressing dNðradÞ with dNðfÞ of (5) yields

dEðradÞ ¼ ��bk�1m ðdq� 3

2qk�1m dkmÞ;

dPðradÞ ¼ �2bk�1=2m ðdq� 3

2qk�1m dkmÞ:

(6)

Energy conservation with (5) and with (6) yields ½ð3��2Þ=ð2�� 2Þ�dkm=km ¼ dq=q, while momentum conser-vation gives ½ð1þ 3�2Þ=ð2þ 2�2Þ�dkm=km ¼ dq=q.

These expressions match for � ¼ ffiffiffi2

p � 1, or kres ¼�ð ffiffiffi

2p � 1Þ2km. As a result, the width and the carrier

wave number of a radiating pulse are related by

qðtÞ ¼ qðt0Þ½kmðtÞ=kmðt0Þ��; (7)

with� ¼ ð3�� 2Þ=ð2�� 2Þ 0:646. Both kmðtÞ and qðtÞincrease as time evolves, and the ratio q=km decays. Thespeed of a pulse decays in time (Figs. 2 and 3). The

expression (7) is equivalent to the solution PðfÞ �NðfÞ ffiffi

8p �3 of (4).

The response of aðradÞk at a fixed k < 0 to the driving forceTk can be computed from (2). A pulse at km drives thismode if k is close to kres ¼ ��2km. The frequency�k has aslow time dependence due to the evolution of the pulse.When�k is close to !k, it can be approximated by a linear

chirp �kðtÞ !k þ _�kt, where _�k � _km=ffiffiffiffiffiffikm

pis small

and changes little near resonance. With aðradÞk ¼bðradÞk expð�i!ktÞ, Eq. (2) is i _bðradÞk ¼ Tk expð�i _�kt

2Þ.Using

R1�1 cosðwt2Þdt ¼ ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi

�=ð2wÞp, the amplitude of the

mode at k will be jaðradÞk j2 � T2k=

_�k or

jaðradÞk j2 � T2k

ffiffiffiffiffiffikm

p= _km (8)

after the driving frequency �k has moved through reso-nance at �k ¼ !k. The amplitude can also be computedfrom conservation of wave action. The pulse that movesfrom km to km þ dkm radiates an amount of wave action

dN � bqk�5=2m dkm into the interval ½��2ðkm þ

dkmÞ;��2km�. Therefore the modes in this interval havethe amplitude

jaðradÞk j2 � qðkmÞk�5=2m : (9)

For the evolution of the carrier wave number, Eqs. (8) and

(9) yield _km � q�1k3mT2k . For the quasisoliton, the feed Tk

to the radiation mode is exponentially small in km=q. For anonlinear pulse, km and q are of the same order, and the

leading order Tk � q2k�9=4m (3) yields _km � q3k�3=2

m .Averaging over the time history of a single pulse as its

wave number increases yields

hjaðfÞk j2i ¼Z t1

t0

jaðfÞk ðkmðtÞ; qðkmðtÞÞÞj2dt

¼Z kmðt1Þ

kmðt0ÞjaðfÞk ðkm; qðkmÞÞj2= _kmdkm: (10)

aðfÞk ðkm; qÞ is the mode at k for a pulse that is centered at km.

The approximation jaðfÞk j2 �ðk� kmÞNðfÞ assumes that

E (f)

P (f)

N (f)1010.1

N (f)

1

0 1000 2000

t3000

0.1

0.5

0.88

0.92

0.96

1(P N ) /E(f)1/2(f)(f)

E /E2(f) (f)

N (f) 0.414

−0.172

(b)(a)

FIG. 5 (color online). (a) The ratios ðPðfÞNðfÞÞ1=2=EðfÞ and

EðfÞ2 =EðfÞ of an evolving pulse as functions of time. (b) Energy

EðfÞ � NðfÞ ffiffi2

p �1 and the momentum PðfÞ � NðfÞ ffiffi8

p �3 of an evolv-ing pulse as functions of the wave action NðfÞ. The wave actionand the energy decrease in time, while the momentum increases.

PRL 103, 074502 (2009) P HY S I CA L R EV I EW LE T T E R Sweek ending

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the whole wave action is localized at km, which yields

hjaðfÞk¼kmj2i ¼ NðfÞ= _km. The peak of the pulse spends an

amount of time dt ¼ dkm= _km between km and km þ dkm.This yields the spectrum

hjaðfÞk j2i � qk�3=2=ðq3k�3=2Þ � q�2 � k�1:29: (11)

Figure 6(a) shows snapshots of the spectrum of a pulse atthree different times and the time-averaged spectrum. Itshows that the central wave number km and the width of apulse increase, while its power decreases. The time-averaged spectrum is in good agreement with the computedpower law k�1:29. This type of spectrum is obtained onlyfor a certain window in wave number space. The relativewidth in wave number space decays, according to (7), as

qðtÞ=kmðtÞ � k��1m ðtÞ. As a consequence, the intensity of

radiation decays and the pulse behaves more like a quasi-soliton, and moves very little in wave number space. Thetime-averaged spectrum decays less rapidly as a functionof k for averages over a very long time.

The simulations also confirm the spectrum of the radia-tion (9). Figure 6(b) shows the spectrum of the radiatedwave action at negative k. For this purpose, damping isapplied to negative k so that the radiation is quickly dis-sipated. The time-averaged spectrum closely matches the

prediction hjaðradÞk j2i � qjkj�5=2 � jkj�1:854 from (9). The

radiation spectrum applies also for quasisolitons with smallq=km.

We have found a turbulent process where radiatingpulses dominate the spectral flow. An open question is,How might one have known, a priori, that the transfermechanisms are dominated by evolving coherent objectsin the MMT equation with � ¼ 1, and by four wave

resonant interactions in the equation with � ¼ �1? Fromexperience to date, coherent objects such as pulses form atall scales only in one-dimensional systems. In dimensiontwo and higher, there are corrections to the KZ spectrum atvery large and very small scales [10,11]. A forthcomingstudy of the breakdown of the wave turbulence picture inone-dimensional systems will investigate instabilities ofthe KZ spectrum under perturbations with correlations.But the challenge of finding a priori general criteria, givenlow-amplitude initial conditions, which distinguish thecircumstances under which resonant waves or coherentobjects dominate the long time dynamics is still open.

[1] V. E. Zakharov, V. Lvov, and G. Falkovich, KolmogorovSpectra of Turbulence (Springer-Verlag, Berlin, 1992);K. Hasselmann, J. Fluid Mech. 12, 481 (1962); V. E.Zakharov and N.N. Filonenko, Dokl. Akad. Nauk SSSR170, 1292 (1966) [Sov. Phys. Dokl. 11, 881 (1967)]; D. J.Benney and P. G. Saffman, Proc. R. Soc. A 289, 301(1966); D. J. Benney and A. C. Newell, Stud. Appl.Math. 48, 29 (1969).

[2] A. J. Majda, D.W. McLaughlin, and E.G. Tabak,J. Nonlinear Sci. 7, 9 (1997); D. Cai, A. J. Majda, D.W.McLaughlin, and E.G. Tabak, Proc. Natl. Acad. Sci.U.S.A. 96, 14 216 (1999); D. Cai and D.W.McLaughlin, J. Math. Phys. (N.Y.) 41, 4125 (2000);D. Cai, A. J. Majda, D.W. McLaughlin, and E.G. Tabak,Physica (Amsterdam) 152–153D, 551 (2001).

[3] V. E. Zakharov, P. Guyenne, A.N. Pushkarev, and F. Dias,Physica (Amsterdam) 152–153D, 573 (2001).

[4] V. Zakharov, F. Dias, and A. Pushkarev, Phys. Rep. 398, 1(2004).

[5] B. Rumpf and L. Biven, Physica (Amsterdam) 204D, 188(2005).

[6] H. Tamura, T. Waseda, and Y. Miyazawa, Geophys. Res.Lett. 36, L01607 (2009).

[7] D. R. Solli, C. Ropers, P. Koonath, and B. Jalali, Nature(London) 450, 1054 (2007).

[8] V. I. Karpman and H. Schamel, Phys. Plasmas 4, 120(1997).

[9] N. Akhmediev and M. Karlsson, Phys. Rev. A 51, 2602(1995).

[10] L. Biven, S. V. Nazarenko, and A. C. Newell, Phys. Lett. A280, 28 (2001); A. C. Newell, S. V. Nazarenko, andL. Biven, Physica (Amsterdam) 152–153D, 520 (2001);L. Biven, C. Connaughton, and A. C. Newell, Physica(Amsterdam) 184D, 98 (2003).

[11] A. C. Newell and V. E. Zakharov, Phys. Lett. A 372, 4230(2008).

10

1

0.1 1

−310

10−2

0.1

0.10.01

|k| |k|

timeaverage

timeaverage

|k||k|

−1.854−1.29

|a | k

2 2|a

| k

t= 500

t=1000

t=2000

(a) (b)

FIG. 6 (color online). (a) Time evolution of a radiating pulse.In wave number space the peak of intensity of the pulse at kmmoves towards higher k. The wave action of the pulse decays.The time average of the evolving pulse yields a spectrum

hjaðfÞk j2i � k�1:29. (b) The radiation emitted by the pulse has a

spectrum hjaðradÞk j2i � k�1:854.

PRL 103, 074502 (2009) P HY S I CA L R EV I EW LE T T E R Sweek ending

14 AUGUST 2009

074502-4


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