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Physica D 63 (1993) 213-232 North-Holland PINSICA 0 Oscillatory convection in a rotating layer E. Knobloch a and M. Silber b a Department of Physics, Universityof California, Berkeley, CA 94720, USA b Department of Applied Mechanics, California Institute of Technology, Pasadena, CA 91125, USA Received 18 June 1992 Accepted 11 August 1992 Communicated by R.S. MacKay The stability of travelling and standing rolls in oscillatory rotating convection is considered from the point of view of equivariant bifurcation theory. To study stability with respect to oblique perturbations the problem is formulated on a rotating rhombic lattice. All primary solution branches with maximal isotropy are determined together with their stability properties using a truncation of the most general equivariant vector field at third order. In addition as many as seven branches of temporally periodic or quasiperiodic solutions with submaximal isotropy may be present. Instabilities analogous to the Kiippers-Lortz instability of steady rolls in rotating convection are uncovered for both travelling rolls and for standing rolls. These instabilities are triggered by the formation of a heteroclinic orbit connecting two travelling roll states or two sets of standing rolls with different wave vectors. Conditions are given for the formation and asymptotic stability of a structurally stable heteroclinic cycle connecting four travelling roll states. The results are compared with recent studies of oscillatory patterns on a rotating square lattice and on a nonrotating rhombic lattice. 1. Introduction Bifurcation theory has been of great value in understanding the selection process among spa- tially periodic patterns in a variety of continuous systems. The main reason for this success is its emphasis on the use of symmetries. The symme- tries in question are those of the periodic lattice on which the patterns lie (either rhombic, square or hexagonal if the system is two-dimensional), together with any normal form symmetry. The trivial state of the system is, by definition, in- variant under this group of symmetries, here- after denoted by I. As a parameter is increased this state loses stability in a symmetry-breaking bifurcation forming a pattern, i.e., a state that is invariant under only a subgroup of I. The possi- ble patterns are thus identified with the isotropy subgroups of the full symmetry group, thereby capturing precisely those properties that patterns in different systems have in common. In addi- tion the requirement that the amplitude equa- tions be equivariant with respect to the appro- priate representation of the full symmetry group r can be used to write down the general form of such equations for all systems with a com- mon symmetry I. Moreover the residual sym- metry of each pattern can be used with advan- tage to simplify the determination of its stabil- ity properties with respect to all the competing patterns on the lattice. These developments have recently been summarized by Golubitsky et al. [ 1 ] and their application to spatially periodic pattern selection in planar systems invariant un- der the Euclidean group E(2) of rotations, re- flections and translations of a plane has been re- viewed by Crawford and Knobloch [ 21. When reflection symmetry is broken so that the system is invariant under translations and proper rotations only, a new phenomenon may arise. This is an instability, discovered by Kiippers and Lortz [3] in their study of con- 0167-2789/93/$06.00 @ 1993-Elsevier Science Publishers B.V. All rights reserved 213

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Page 1: E. Knobloch, M. Silber / Oscillatory convection in a rotating layer 215tardis.berkeley.edu/reprints/papers/KnSi_PD63_1993.pdf · 2015. 5. 13. · 214 E. Knobloch, M. Silber / Oscillatory

Physica D 63 (1993) 213-232 North-Holland PINSICA 0

Oscillatory convection in a rotating layer

E. Knobloch a and M. Silber b a Department of Physics, University of California, Berkeley, CA 94720, USA b Department of Applied Mechanics, California Institute of Technology, Pasadena, CA 91125, USA

Received 18 June 1992 Accepted 11 August 1992 Communicated by R.S. MacKay

The stability of travelling and standing rolls in oscillatory rotating convection is considered from the point of view of equivariant bifurcation theory. To study stability with respect to oblique perturbations the problem is formulated on a rotating rhombic lattice. All primary solution branches with maximal isotropy are determined together with their stability properties using a truncation of the most general equivariant vector field at third order. In addition as many as seven branches of temporally periodic or quasiperiodic solutions with submaximal isotropy may be present. Instabilities analogous to the Kiippers-Lortz instability of steady rolls in rotating convection are uncovered for both travelling rolls and for standing rolls. These instabilities are triggered by the formation of a heteroclinic orbit connecting two travelling roll states or two sets of standing rolls with different wave vectors. Conditions are given for the formation and asymptotic stability of a structurally stable heteroclinic cycle connecting four travelling roll states. The results are compared with recent studies of oscillatory patterns on a rotating square lattice and on a nonrotating rhombic lattice.

1. Introduction

Bifurcation theory has been of great value in understanding the selection process among spa- tially periodic patterns in a variety of continuous systems. The main reason for this success is its emphasis on the use of symmetries. The symme- tries in question are those of the periodic lattice on which the patterns lie (either rhombic, square or hexagonal if the system is two-dimensional), together with any normal form symmetry. The trivial state of the system is, by definition, in- variant under this group of symmetries, here- after denoted by I. As a parameter is increased this state loses stability in a symmetry-breaking bifurcation forming a pattern, i.e., a state that is invariant under only a subgroup of I. The possi- ble patterns are thus identified with the isotropy subgroups of the full symmetry group, thereby capturing precisely those properties that patterns in different systems have in common. In addi-

tion the requirement that the amplitude equa- tions be equivariant with respect to the appro- priate representation of the full symmetry group r can be used to write down the general form of such equations for all systems with a com- mon symmetry I. Moreover the residual sym- metry of each pattern can be used with advan- tage to simplify the determination of its stabil- ity properties with respect to all the competing patterns on the lattice. These developments have recently been summarized by Golubitsky et al. [ 1 ] and their application to spatially periodic pattern selection in planar systems invariant un- der the Euclidean group E(2) of rotations, re- flections and translations of a plane has been re- viewed by Crawford and Knobloch [ 21.

When reflection symmetry is broken so that the system is invariant under translations and proper rotations only, a new phenomenon may arise. This is an instability, discovered by Kiippers and Lortz [3] in their study of con-

0167-2789/93/$06.00 @ 1993-Elsevier Science Publishers B.V. All rights reserved 213

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214 E. Knobloch, M. Silber / Oscillatory convection in a rotating layer

vection in a rotating fluid layer, that causes a steady roll pattern to be unstable with respect to an identical pattern rotated through some angle 8 (in the corotating frame of reference). Such an instability is absent in a nonrotating system and requires the rotation rate to exceed a criti- cal value. Note that for low rotation frequencies the centrifugal force may be neglected so that rotation manifests itself primarily through the Coriolis force [ 41. Consequently, the system re- mains invariant under translations and proper rotations, but not reflections; the symmetry of the problem is then that of the special Euclidean group SE(2).

To understand the origin of the Kuppers- Lortz instability consider a steady state bifurca- tion on a rhombic lattice defined by the funda- mental lattice vectors ai, a2 such that a I - u2 =

~a~~~a2~cost9 with Iail = Ia21 = 2x/k,. Here k, is the critical wavenumber of the instabil- ity. Any smooth field w (x, y, t) describing the state of the fluid and satisfying the periodicity requirement

w(x + n1a1+ n2aaz,.Y,t) = vvx,Y,t),

(h, n2) E z2, (1)

can be written in the form

w=F zmn(t) e i(mkl+nk2bx y,, ty)

m,n=O

+ C.C. (2)

Here ki*aj = 2K6ij, i, j = 1,2, and Y,,(y) de- notes the vertical structure of the (m, n&mode. Near onset we write

v/ = (zi eikl’X +z2 e*““)Y(y) + ._.

+ C.C. (3)

with the amplitudes of the higher order modes slaved to the evolution of the amplitudes zl, ~2.

In a system invariant under proper rotations and

translations, the symmetry group associated with patterns doubly-periodic on a rhombic lattice is Z, x T2, where Z, corresponds to a rotation by n and T2 is the two-torus of translations. The symmetry group Z, x T2 acts on ( z 1, z2 ) E C2 as follows:

rotation x -+ --x :

(ZlJ2) - Gl32),

translations n -+ x + d :

(z,, z2) + (zl eikl.d, z2 eik2’d). (4)

The amplitude equations are equivariant with respect to these operations and hence take the form

ii = fi (2, lz,12, Iz212h 3

i2 = .f2(& lz,12, lz212b2 > (5)

where A is the bifurcation parameter, and J;, j = 1, 2, are real functions that satisfy the additional constraint fi (2, U, 0) = f2 (&O, u). This con- straint follows from the SO(2) c SE(2) invari- ance of the original physical problem: the evolu- tion equations for pure rolls in the k 1 -direction (~2 = 0) must agree with those obtained for pure rolls in the kz-direction (zi = 0). In terms of the real variables zj = rj e’$J, j = 1,2, we therefore have

ii = Art + urf + brirl + . . . , 4, = 0,

i2 = ;1r2 + crfr2 + ar,3 + . . . , $2 = 0, (6)

near A = 0. Pure rolls correspond to solutions with (rl,rz) = (r,O), or (r1,r2) = (O,r), r2 = --A/a (hereafter R 1, R2, respectively). The sta- bility properties of these two sets of rolls are not identical. This is because the presence of the Coriolis force breaks the reflection symmetry (zi, z2) + ( z2, z1 ) that forces the coefficients b, c to be identical in a nonrotating system. If

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E. Knobloch, M. Silber / Oscillatory convection in a rotating layer 215

Fig. 1. Typical phase portraits showing the formation of the heteroclinic orbit responsible for the onset of the Kiippers-Lortz instability of steady rotating convection. (a) The nonrotating case (b = c < a < 0), with the stable and unstable manifolds of the mixed mode indicated in the (rl, rz)-plane. (b) The rotating case, no Kiippers-Lortz instability (b < c < a < 0), and (c) the rotating case with a Kiippers-L.ortz instability from RI to R2 (b < a < c, a < 0). The mixed mode no longer exists.

a < 0 so that both sets of rolls bifurcate super- critically, the stability of rolls RI with respect to perturbations in the form of R2 is determined by sgn(c - a ), while the sign of the corresponding eigenvalue of R2 is given by sgn (b - a ) . For slow rotation (b x c) both eigenvalues are negative, but for large enough rotation c - a becomes pos- itive with the result that RI are now unstable to Rz, and by the same argument R2 are unstable to a third set of rolls again at an angle 8, etc. The rotation rate at which this instability first sets in for some angle 8 was calculated by Kiippers and Lortz for rotating Rayleigh-BCnard convection with stress-free boundaries [ 31, and by Kiippers for no-slip boundaries [ 5 1. Mathematically, the instability sets in when an unstable mixed mode (ri , r2), ri # r2, ri rz # 0, annihilates with RI in a subcritical pitchfork bifurcation, forming a het- eroclinic orbit connecting RI to R2 (see fig. 1). This first occurs for a particular angle 8 which we choose to define the lattice. For more details, see Knobloch and Silber [ 61. The resulting insta- bility has been observed experimentally [ 7,8].

The present paper is motivated by the above scenario. We seek analogous instabilities in a rotating system undergoing a Hopf bifurcation. Our analysis is pertinent to rotating Rayleigh- BCnard convection in low Prandtl number fluids; a linear analysis shows that in such a fluid the spatially uniform heat conduction state may lose stability via Hopf bifurcation if the rotation rate is sufficiently great [ 41. In an earlier paper [ 9 ]

we describe the analogue of the Kiippers-Lortz instability for travelling rolls on a rotating square

lattice (8 = a/2). The instability takes the form of a structurally stable attracting heteroclinic cy- cle connecting waves travelling in four orthogo- nal directions. A similar instability for standing rolls is, however, prohibited for the square lat- tice. In this paper we generalize the discussion to a Hopf bifurcation on a rotating rhombic lattice. We find that there are as many as eleven primary solution branches that bifurcate at the Hopf bi- furcation. Four of these are always present and are periodic in time. Existence of the remain- ing seven depends on the values of the cubic co- efficients; four of these solutions correspond to temporally-periodic standing wave patterns, two correspond to quasiperiodic travelling patterns, while the remaining solution corresponds to a quasiperiodic standing wave. We compute the stability properties of the four solutions that al- ways exist, as well as those of the two quasiperi- odic travelling patterns. We focus on Kiippers- Lortz type instabilities for both travelling and standing rolls, and identify a structurally stable heteroclinic cycle between travelling rolls.

The paper is organized as follows. In section 2 we present the group-theoretic analysis of the problem, constructing the lattice of isotropy sub- groups that describes the possible symmetries of patterns on the rotating rhombic lattice. In section 3 we construct the amplitude equations, truncated at third order, and compute explicitly

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216 E. Knobloch, M. Silber / Oscillatory convection in a rotating layer

the primary branches. In section 4 we investigate their stability properties. In section 5 we deter- mine the possible heteroclinic cycles in our sys- tem and investigate the possibility of a primary bifurcation to a quasiperiodic standing wave so- lution. In the last section we compare our re- sults to those for the rotating square lattice [9] and the nonrotating rhombic lattice [lo]. We also discuss the relationship between the rotat- ing rhombic lattice and the rotating hexagonal lattice [ 111. Finally, we discuss the application of our analysis to spatially periodic pattern for- mation in rotating convection.

2. Group-theoretic considerations

The symmetry group for patterns doubly- periodic on a (rotating) rhombic lattice is Z, x T2, where Z, is the reflection group gen- erated by rotations of the lattice by n and T2 is the two-torus of translations (cf. eq. (4) ). When the initial instability is a Hopf bifurca- tion near-identity nonlinear coordinate changes can be performed to put the resulting amplitude equations into PoincarbBirkhoff normal form. This normal form has an additional S’ tempo- ral symmetry, which we refer to as the phase shift symmetry. In the following we therefore as- sume that the symmetry group of the problem is F~Z2xT2xS1.Atonsetwewrite (cf.eq. (3))

v(x,y,t) = (z,(t) eik1’x +z2(f) eik2’X

+zs(f) e-ikt.x +zq(t) e-ik2’X)Y(y)

+ . . . + C.C., (7)

and assume that the linear stability problem takes the form i = ~(1) z, where z = (z ,,

z~,zJ,z~) E C4, and ~(0) = iw,, Re($(O)) > 0. Here A is the bifurcation parameter. It follows that the quantities (]zi],]zs]) and (122/,]241) represent amplitudes of left- and right-travelling waves in the k , , k2 directions, respectively. To understand how the group F acts on z E C4 we consider the effect of translations x + n + d,

and of rotations x --+ --x on the critical Fourier modes. We also assume an overall phase shift symmetry associated with the normal form for Hopf bifurcation [ 121; this symmetry is inter- preted as a time translation symmetry of peri- odic solutions with frequency 52: t --+ t + qb js2.

From (7) it follows that these operations are equivalent to the following action of F on C4:

K: K Ez2,

/ZI \ / eiel z1 \

("1,02) E T2,

@z-e , i# z q+E s’. (8)

Here the phase shift 6, results from a translation in a direction perpendicular to k2; similarly the phase shift 02 is a consequence of translating in a direction perpendicular to k 1. We note that this representation does not force the Fourier modes ~2, z4 to undergo a Hopf bifurcation when zl, z3

undergo one: (8) is not the generic type of rep- resentation associated with equivariant Hopf bifurcation problems (see [ 1 ] ). It arises here, in a generic bifurcation problem, because of the SO (2 ) c SE (2 ) invariance of the physical prob- lem prior to the imposition of periodic bound- ary conditions. We also observe that the phase shift 4 = rr E S’ acts on C4 in the same way as a mid-plane reflection symmetry does in the case of Boussinesq convection with identical bound- ary conditions at the top and bottom of the fluid layer (see, for example, ref. [ 131). Thus the normal form for the Hopf bifurcation is the same when the mid-plane reflection symmetry is present as it is when this symmetry is absent.

The vector field i = f (z), which governs the dynamics of the critical modes on a neigh-

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E. Knobloch, M. Silber / Oscillatory convection in a rotating layer 217

borhood of the Hopf bifurcation, must be I- isotropy subgroup is a linear subspace Fix(Z), equivariant: which is invariant under the dynamics ( 10):

of = f(yz), for all y E r. (9)

Equivariance with respect to T2 x S1 determines the form of it and iz [ 141. Equivariance with respect to Z, then generates i), id from ii, iz, respectively. It is thus straightforward to show that a smooth vector field commuting with the above symmetries has the form

ii =p(lzi12, lz212, lz312, lz412, Q)zl

+ 4(lz*12, lz212, Iz312, l~412,m2~4~3

i2 = r(lz112, lz212, lz312, lz412mz2

+ Nz,12, 1~21~5 lzd2, lz412, Qlz1~3Z4

23 =P(Iz~I~, lz412> b,12, b212> Qb3

+ d1z312, 1z412, )z112, Iz212,t%2z4-%

Fix(X) = {z E C4 : oz = z,Va E C}. (12)

Hence all solutions with symmetry C c I’ evolve under ( 10) restricted to the subspace Fix(C). In table 1 we list all the isotropy subgroups of r (up to conjugacy) together with their fixed point subspaces. We may identify solutions in Fix(C) with spatio-temporal patterns using the expres- sion (7 ). Note, however, that (7) represents the linear solution, which provides a good descrip- tion of the pattern close to onset only, while the classification of the patterns in terms of the isotropy subgroups is valid even in the presence of nonlinearities. (See [ 15 ] for a discussion of linear steady rotating convection patterns that have more symmetry than expected from a di- rect calculation of the appropriate isotropy sub-

group. 1

i4 = r@312, lz412, lh12, lz212,a’)z4

+ dlz312, lz412, lz112> lz212, Q)zlz3?2,

(10)

where Q = z1~zz~‘L4, and p, q, r and s are complex-valued functions of their arguments and of the bifurcation parameter 1. Moreover, because of the SO(2) invariance of the original problem, the functions p and r are related by the constraint p(u,O,v,O,O) = r(O,u,O,v,O). We now summarize the information about the possible periodic solutions to ( 10) that can be obtained using group-theoretic arguments alone.

Each nontrivial (pattern-forming) solution z # 0 breaks the full symmetry I, and there- fore has symmetry characterized by an isotropy subgroup C, of I?

c, = {a E 1-: fsz = z}. (11)

The successive breaking of the full symmetry is summarized by the lattice of isotropy sub- groups of I shown in fig. 2. Associated with each

The equivariant Hopf theorem guarantees the existence of primary solution branches with two- dimensional fixed point subspaces [ 12 1. In the present case these are the travelling rolls (TRt ,

TR2 ), and the standing rolls (SRI, SRz ). We note that for the rotating square lattice prob- lem (with Z, x T2 x S’ symmetry) the equiv- ariant Hopf theorem determines the existence of two additional primary branches, referred to as standing squares (SS) and alternating rolls (AR) [9]. In the case of the nonrotating rhom- bic lattice (with Dz x T2 x S’ symmetry), the equivariant Hopf theorem guarantees two trav- elling rectangle patterns in addition to TR, SR and AR, the SS, which become standing rectan- gles, must also exist [ lo]. All of these solutions are periodic in time. Note also that the rotat- ing rhombic lattice problem approaches the ro- tating square lattice problem as 8 + 7r/2. Sim- ilarly, as the rotation rate goes to zero, the dis- crete symmetry of the problem increases from Z, to D2, the symmetry group of a rectangle. All of these problems may thus be viewed as per- turbations of the Hopf bifurcation problem with

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218 E. Knobloch. M. Silber / Oscillatory convection in a rotating layer

CT)

A\\ SO(Z) x S%(2) zz x i* x SO(2) SO(Z) x S?)(2) z* x iz x SO(2)

(Th) (SRI) (TRz) (S&l

\\ i* x SO(2) ST3 2) S3(2) i, x SO(2)

(MRI) (T%) (TBz) (& (Mfh)

\w

(Q?3)

Fig. 2. Lattice of isotropy subgroups. Arrows indicate inclusion. Isotropy subgroups are described in tables 1 and 2.

Table 1

is contained in every Z.

Fixed point subspaces corresponding to (zt, ~2, zs, zq) as in (7), each wi E C, j

the different isotropy subgroups of I. The coordinates specifying each Fix(Z) are = 1, 2, 3, 4. Table 2 describes each isotropy subgroup ZL The trivial symmetry Z,’

Name Fix(Z) z

0

I

II

III

IV

V

VI

VII

VIII IX X

trivial solution (T) travelling rolls (TR, )

travelling rolls (TR;, )

standing rolls (SRI ) standing rolls ( SR2 )

modulated rolls (MR , ) modulated rolls ( MR2 )

travelling bimodal (TB , ) travelling bimodal (TB2 ) standing bimodal (SB) triply periodic (QP3)

z = (O,O,O,O)

z = (~1,0,0,0) z = K4v,,O,O) z = (Vl,O,V,,O)

z = (0,v,,0,v,)

z = (~I>O>~Z,O)

z = (O,Vl,O,V2)

z = (v1,v2,0,0)

z = (~1>0>0,~2)

z = (~1,~2,~1,~2)

z = (vI,v2,v3,v4)

I-

SO(2) x So?2)

SO(2)_x So?2)

z, x c2 x SO(2) L2 x z, x SO(2)

52 x SO(2) Z,SO(2)

SO(2) So(2)

z2

H2C

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E. Knobloch, M. Silber / Oscillatory convection in a rotating layer 219

Table 2 Generators of isotropy subgroups in table 1. Group elements of T* x S1 are denoted [ (&, I%,), 41, where (O,, 02) E T* and dE.5’.

z Generators of C

TR1

TR2

SRI

SR2

MRI MRz TBI TB2

SO(2) x 675)

SO(2)x 55)

z* x c* x SO(2)

h_z x z, x SO(2)

z_z x SO(2) hESO@) SO@) S6j5) z2

z2c

[(o,e),oi ESO(~), [(e,o),-ei ~~67%

[(e,o),oi E SO(~), [0,0),-e] E SO(~)

K E z2!2, I(n,O),nl E 2, I(o,e),oi E SO(~) K E z,, I(O,n),nl E z*, I(e,o),ol E SO(~) I(%u),al ES, I(o,e),oi E SO(~) [to, n), aI E z*, I(e,o),oi E SO(~) I(e,e),-01 E SO(~) [(e, 4, -ei E so?z)

K E z,

I(n,II),al E z,c

D4 x T2 x S’ symmetry analyzed in detail by Sil- ber and Knobloch [ 141. Moreover, most of the submaximal isotropy solutions that are found in the next section may be understood as continua- tions of maximal isotropy solutions of the nonro- tating rhombic lattice problem analyzed by Sil- ber et al. [lo].

3. The amplitude equations and primary branches

The coefficients p, a, b, c, d, e, f, g and h are all complex. In the following we suppose without loss of generality that p(A) = A+ io, where w - w, = 0 (A) and oC is the Hopf frequency at A = 0. We note that for the rotating square lattice there is an additional a/2 rotational symmetry that forces (c,d,e) = (g, f,h) [9], whereasfor the nonrotating rhombic lattice reflection sym- metryguaranteesthat (c,d,e) = (f,g, h) [lo]. In the case of a nonrotating square lattice c = d = f = gande = h [14].

In the following we expand the functions p, q, r and s in ( 10) in a Taylor series about the origin, and truncate the resulting equations at cubic order:

The small amplitude temporally-periodic solu- tions created at the Hopf bifurcation satisfy the equation i = iQz, where the frequency 52 x wC is to be determined. Thus they satisfy the alge- braic equations

ii =PzI + (alz112+b1z3~2+C~z2~2+d~z4~2)Z1

+ ez2.2453,

vzl + (alz112 + blz3j2 + clz212 + dlz412h

+ez22473 = 0,

22 =pz2+ (~lz212+blz412+flZ1~2+glz312)Z2

+ hZ1Z324,

vz2 + blz212 + blz412 + flz~l~ + glz312)z2

+hzlz3T4 = 0,

i3=pz3+ (~lz312+blz,12+Clz412+dlz212)z3 vz3 + (alz312 + blz112 + clz412 + dlz212b3

+ ez2z471, +ez2z4Z1 = 0,

i4=Pz4+ (~lz412+blz212+flZ312+glZ,12)Z4

+ hZ*Z3T2. (13)

vz4 + @lz412 + blz212 + flz312 + glzd2)z4

+hZ*Z3T2 = 0, (14)

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220 E. Knobloch, M. Silber / Oscillatory convection in a rotating layer

where Y = p (2) - is2. There are four solutions that reside in the two-dimensional fixed point subspaces. These take the form of travelling and standing rolls in the k;-directions (j = 1,2), hereafter denoted by TRj and SRj:

TR, : (~,O,QO), v + a/?J/2 = 0,

TR2 : (O,v,O,O), Y + a17g = 0,

SRI : (r.r,O,%r,O), U + (a + b)JV)2 = 0,

SR2 : (O,TJ, o,u ), v + (a + b)ll# = 0.(15)

These solutions have maximal isotropy (cf. fig. 2) and their existence is guaranteed by the equivariant Hopf theorem [ 121. The branching equations are identical for each of the TRj and each of the SRj because of the underlying SO (2 ) symmetry of the unrestricted problem. How- ever these pairs are not related by a symmetry associated with the rhombic lattice.

We next examine the dynamics in each of the four-dimensional fixed point subspaces listed in table 1 (entries V-IX). The dynamics in the modulated rolls subspaces (MRi , MR2) are the same as in the O(2) Hopf bifurcation prob- lem. This is readily verified by setting z = (11r,O,212,0) and z = (0,2ri,O,~) in (13) to obtain

v2 = ,mJ2 + (alv212 + b~v~~2)u2. (16)

Generically, the only nontrivial periodic or quasiperiodic solutions in this subspace are TR and SR [ 121. Thus there are no new solution branches associated with the MRt and MR2 subspaces.

Associated with the four-dimensional lixed point subspace z = (zI,, 212,0,0) is a quasiperi- odic solution called a travelling bimodal pattern (TBr ). The TBi take the form (zt, ~2, zs, zq) = (eiQIf5 , i eiQzl 62, 0,O). The amplitudes /Cj] and frequencies Qj, j = I, 2, are determined by

q + uliQ2 + cIG212 = 0,

v2 + @212 + flG,12 = 0, (17)

where vj = p - iQj. Written in terms of their real and imaginary parts eqs. ( 17) become

A + UrlG12 + CrIV212 = 0,

A + Ur1%1212 + f,lG12 = 0,

W -sZl + UiliT112 + CilV212 = 0,

W - s22 + UilC212 + J;111112 = 0, (18)

where the r and i subscripts specify the real and imaginary parts of the coefficients. The first two equations are identical to those for the steady state patterns on the rotating rhombic lattice (cf. equation 6). It follows that TBt are given by

1% I2 ( > -A a, - cr Ia2 = a;-c,fr a,-fr ; ( > (19)

the last two equations of ( 18) determine the cor- responding frequencies (Qt , i22 ) . Note that these solutions exist if and only if a, - cr and a, - Jr have the same sign, and hence are not present for all coefficient values.

The TB2 take the form (z~,z~,.zT~,z~) =

( einl f 17,) 0, 0, eiQzl V2 ), where

v1 + uIG,)~ + dlV2j2 = 0,

23 + ulv212 + g@12 = 0. (20)

The branching equations and the corresponding frequencies can both be deduced from those for TBi on letting (c,f) -+ (d, g). Thus TB2 exist if and only if (a, - d, ) (a, - gr ) > 0.

Next we consider the existence of more com- plicated but periodic solutions in the standing bimodal subspace tained by setting z ing the equations

(SB). Such solutions are ob- = (~i,v2,2)~,2)~) in (13) yield-

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E. Knobloch. M. Silber / Oscillatory convection in a rotating layer 221

G =w1 + (a + b)(lv112 + 1~212)~1

- 4v21221, + ev1&

212 =pJ2 + (a + b) (Iv112 + Iv212)v2

- nlu112v2 + hv3J.2,

where

(21)

m=a+b-c-d, n=a+b-f-g. (22)

Following Swift, we introduce the coordinate transformation [ 161

v1 = fi cos(8/2) ei(P+w)/2,

212 = fi sin(f3/2) ei(-g+w)/2, (23)

where8E [O,rr],andq,,vE [0,2a).Duetothe S* symmetry of (2 1 ), the @ equation decouples from the following equations for r, 8, Q:

i = 2r(A + rgo(8,y,)),

4 = rsin8 gl(e,p),

V; = rg2ce,d,

where

go =a, + b, - isin’

xRe(m+n-ee -2i(o _h e2iP) ,

gl = sin2(0/2) Re(m - e ee2i9)

- cos2(8/2) Re(n - h e2@) 7

g2 = - sin2(8/2) Im(m -e ee2j9)

+ c0s2(e/2) Im(n -h e2’9).

(24)

(25)

Note that the vector field (24)-(25) is invari- ant under a, -+ p + n. This symmetry is a mani- festation of the translation symmetry (vl ,212 ) +

(211, -212) of (2 1) in the spherical coordinates (23). By introducing the new time r that satis- ties r = r, r(0) = 0, we obtain the following dynamical system on the sphere S2:

8’ = sine glMp), V’ = g2md, (26)

where ’ denotes differentiation with respect to r. A fixed point (t-o,&, ~0) of (24) corresponds to a periodic solution of ( 13) since @ = 20 + . . . .

Note that the bifurcation parameter A does not appear in (26). Whether a periodic solution in the SB subspace bifurcates supercritically or sub- critically is determined by the sign of go (80, qo)

in the i equation since

r0 = -A/g0 (60, q0) > 0. (27)

The periodic solutions SRt, SR2 appear as fixed points of (26) at the north and south poles (8 = 0, n ) . All other periodic solutions in the SB subspace correspond to solutions of gl (0,~) = g2 (8, Q ) = 0. From these conditions we obtain the following two equations for tan2 (e/2):

tan2(8/2) = Re(n - h e2@)

Re(m -e e-2i9) >o

Im(n -h e2@)

= Im(m -e e-2i9) >o. (28)

Thus for submaximal periodic solutions to exist in the SB subspace, there must exist a v, satisfying the equation

Im[(n-h e2i9)(m-V e2”)] = 0, (29)

subject to the requirement tan2 (e/2) > 0. The existence conditions (28)) (29) have the follow- ing geometric interpretation if we view n -h e2i9 and m - e ee2@ as vectors in the complex plane. Equation (29) specifies that for some angle Q the vectors must be parallel (or antiparallel) for a solution to exist. The inequalities then rule out the case where the vectors are antiparallel. Given this interpretation, it is straightforward to find regions of the (m, II, e, h )-coefficient space where no submaximal periodic solutions exist (see, for example, fig. 3 ) . Some of the interest- ing dynamics associated with these regions are examined in section 5.

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222 E. Knobloch. M. Silber / Oscillatory convection in a rotating layer

Im Im

h m e @=-I@ ” Re

(4 (b)

Fig. 3. Possible points n-h e2@ and m-e em2’p are plotted in the complex plane for all values of (p E [0, A 1. Note that vectors from the origin to points on the two circles are never parallel. In (a) gt (0, q~) > 0 in (26) for all values of 6, q, and in (b) g2 (0, a) < 0. In both cases, no submaximal periodic solutions exist in the SB subspace.

A complete classification of the solutions of (29) in the (m, n, e, h)-coefficient space is be- yond the scope of the present paper. However, in the special case where m = n, e = h the dy- namics of the associated spherical system (26) have been determined [ 161. In this case there are either two or four distinct solutions, each of which comes in a symmetric pair because of the symmetry q + a, + n of (25): one of the pair is in the hemisphere v, E [0, rc) and the other sat- isfies v, E [rr, 27~). For these special coefficient values the solutions satisfy the equations

sin2y, []e12cos2y, -Re(mP)] = 0,

tan2(8/2) = Re(m -e e2@)

Re(m -e e-2ip) > 0. (30)

The two pairs of solutions that always exist are on the equator of the sphere (0 = 71/2) and satisfy

(SS): (0 = O,n, (AR): v, = n/2,371/2. (31)

Moreover, if [ml2 > lej2 > ]Re(me)] then there are two additional pairs of solutions satisfying

Re(mP) (SCR): cos2~ = le,2 , (32)

p+ c3 ss AR

scfl**

3

Ia) (W

Fig. 4. Fixed points corresponding to the periodic so- lutions SS, AR, SCR and SR in the spherical system (26) for m = n, e = h. In (a) the SCR solutions do not exist, and in (b) two distinct SCR solutions exist (lrn12 > Je12 > IRe(mZ

with tan2 (0/Z) given by (30). One symmetric pair is in the northern hemisphere (tan (f3/2 ) <

1) and the other pair is in the southern hemi- sphere (tan(8/2) > 1) (see fig. 4). We now use the implicit function theorem to show that these solutions persist for (m, e) sufficiently close to (n, h ). Specifically, let

g(e,v;m,n,e,h)

= (gl(8,~;m,n,e,h),g2(e,~;m,n,e,h)),

(33)

where SS, AR and SCR satisfy g (0, v; m, m, e, e) =O,andletDg(B,q;m,n,e,h)bethe2x2 Jacobian matrix associated with g. Then

Det(D~W4~;m,m,e,e))

= -2sine[cose sin2a,Im(me)

+ cos2yl (Re(mi?) - le12cos2v)]. (34)

The determinant (34) is nonzero when eval- uated on the SS, AR solutions provided (Re(mF)l # le12. M oreover, the determinant is always nonzero when evaluated on the SCR solution since ]Im( me) ( # 0 follows from the existence condition /ml2 > le12 > ]Re(mc)]. Thus the implicit function theorem applies and the (perturbed) SS, AR and SCR solutions con-

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E. Knobloch. M. Silber / Oscillatory convection in a rotating layer 223

tinue to exist on a neighborhood of (n,h) = (m, e). Recall that for the rotating square lattice (g,f,h) = (c,d,e) [9] and for the nonrotat- ingrhombiclattice (g,f,h) = (d,c,e) [lo] so that in both of these cases (n,h) = (m,e) on the SB subspace. In each of these cases the exis- tence of SS and AR is guaranteed by the equiv- ariant Hopf theorem. (In the latter case the SS solution corresponds to a standing rectangle pattern.) It follows from these observations that either two or four distinct standing bimodal so- lutions always bifurcate from the trivial solution if the angle 8 is sufficiently close to a/2 or if the rotation rate is sufficiently slow.

4. Stability results

In this section we discuss the stability prop- erties of the four primary branches whose exis- tence is guaranteed by the equivariant branching lemma. We also compute the stability properties of the travelling bimodal patterns.

The technique used in establishing the stabil- ity of the various patterns has been described in detail by Silber and Knobloch [ 141. It relies on the isotropy subgroup of the solution to con- struct the isotypic decomposition of R8 for that solution [ 11. In the coordinates suggested by this decomposition the 8 x 8 Jacobian matrix is then block-diagonal. Additional restrictions imposed by the full symmetry r can be used to deduce the number of zero eigenvalues and to constrain the structure of the blocks even further. We omit the details and summarize the results in table 3.

The travelling rolls TRi , TR2 each have a sin- gle zero eigenvalue associated with the phase shift symmetry. The stability with respect to am- plitude perturbations is given by sgn a,. The re- maining 6 eigenvalues come in complex conju- gate pairs and are associated with eigenvectors in the TBi, TB2 and MRj subspaces, i = 1 or 2, respectively. The SRj (j = 1,2) in contrast have two zero eigenvalues associated with neu- tral stability under translation in the kj direc- tion and under phase shifts. The stability with

respect to amplitude perturbations is given by sgn (a, + b,). Stability Of SRj with respect to TRj perturbations is determined by sgn (a, - b,), as in the Hopf bifurcation with O(2) symmetry. There are two additional eigenvalues associated with eigenvectors in the SB subspace; the sym- metry of the problem forces these eigenvalues to each have multiplicity 2. Note that it is possible for all four of these branches to bifurcate super- critically and yet none be stable.

The possibility of the quasiperiodic (two- frequency) patterns called travelling bimodal patterns was first noted by Knobloch and Silber [9] in their study of the Hopf bifurcation with Z, x T2 symmetry. These patterns do not exist for all coefficient values. Their stability proper- ties are not hard to establish. We describe here the calculations for TBi; the results for TBz are obtained by interchanging the coefficients c and d and the coefficients f and g.

We determine the linear stability of the TBi solution by setting z = ((21 + ~1) eiRlr, (22 + 212 ) eiR21, 53 eiQsf, Yd eiQ4’ ) in ( 13)) where the Zj represent perturbations of the TBt solution with (vi(,It~(,Qi,Q2 given by (18). We choose the frequencies Qg, Q, such that 52i -Q + Sz, -s2, = 0. The stability problem in the TB1 subspace is determined by setting Z3 = & = 0 and lineariz- ing about Zl = Yz = 0. We obtain

+ CVi&

+ fw2%, (35)

together with their complex conjugates. There are two zero eigenvalues associated with trans- lation symmetry and phase shift symmetry. The remaining two eigenvalues (sI, s2 ) satisfy

s1 + s2 = 2ar((w12 + Iv212L

SlS2 = 4(a,2 - Gf,)l~1121~212. (36)

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224 E. Knobloch, M. Silber / Oscillatory convection in a rotating layer

Table 3 The branching equations and stability assignments for six of the possible patterns. The quantities m and n are defined in (22). A solution is stable if the signed quantities are all negative. A single asterisk indicates a complex conjugate pair of eigenvalues; a double asterisk indicates eigenvalues of multiplicity two. The eigenvalues S* are given in (38); zero eigenvalues are not listed.

Name

T

TRI

TR2

SRI

SR2

TBI

TB2

Branching equation

1 + ar1711 I2 = 0

1 + aFlu, I2 = 0

1 + (a, + br)lvl12 = 0

1 + (a, + br)lu112 = 0

I + a&J, I2 + crlt1212 = 0 1 + a,17~212 + I;lv~12 = 0 1 + arlul12 + 41121~ = 0 1 + a,lo212 + grlul12 = 0

stability

1 (8 times) sgna,, sgn(b, - a,)‘, sgn(.L - a,)*, sgn(g, - ar)* war, sgn(br - a,)*, sgn(c, - a,)*, sgn(4 - a,)* sgn(a, + b,), sgn(a, - b,), sgn(st + 32) = -sgn n;*, - sgnslS2 = sgn(lh12 - jn12)** sgn(a, + b,), sgn(a, - b,), sgn(st + s2) = -sgnm:*, - sgn,sls2 = sgn(le12 - lm12)** sgntst + ~2) = sgna,, -sgn sls2 = sgn(c,f, - af), sgnRe(s*)* sgn(s, + ~2) = sgna,, - sgn sls2 = sgn(d,gr - a;), sgnRe(s*)*

The linear stability problem out of this fixed point subspace (Zt = Z, = 0) is given by

24 = (P - iQ4 + blu212 + glvl12)Z4

+ hv,TT2F3. (37)

These equations have time-independent coefli- cients, and hence the four eigenvalues s*, S* are readily found:

P ;1

= m,2 - 4, Car - br + _L - gr) (a, - cr)

+ (a, - br + cr - 4) (a, - .L)

*[(tar-cr)(br-a)- tar-fr)(br-4)

-hi (Ur - fr) + ini (U, - Cr))2

+4eh(u,-c,)(u,-f,)l”2 +iQ, >

(38)

where m, n are given by (22 ) . Here L2 is a purely real quantity, and so does not affect the stabil-

ity properties. Note that the quantity under the square root is complex so that the condition for stability, Re(s*) < 0, is no longer simple.

These results have a number of consequences. Since TBt exist only when (a, - c, ) (a, - fr ) > 0 and TB2 exist only when (a, - 4) (a, - g,) > 0, it follows that both TBt and TB2 are present simul- taneously only when TRt and TR2 have identi- cal stability properties. Moreover if a, - cr > 0, then TBi is supercritical only if a,’ - crfr < 0, in which case it cannot be stable, and similarly for TB2. On the other hand if a, - cr < 0, then TBi are supercritical only if uf - c,fr > 0, in which case their stability depends on the eigenvalues S* describing the perturbations out of the TBt fixed point subspace. In the simpler case of the nonrotating rhombic lattice the TB states are pe- riodic (Qt = G?,) and correspond to travelling rectangle solutions. Since in this case these states can be stable [ lo], it follows by continuity of the eigenvalues that the TB states on the rotat- ing rhombic lattice can also be stable, at least for sufficiently slow rotation rates.

We observe, finally, that the SS and AR states can both be stable for a range of coefficient

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E. Knobloch, M. Silber / Oscillatory convection in a rotating layer 225

values on the rotating square lattice [9] and on the nonrotating rhombic lattice [ lo], where their existence is guaranteed by the equivariant Hopf theorem. Moreover, it is possible for both of them to be stable simultaneously or for one of them to coexist stably with the SR solutions [ 9,101. Both AR and SS have three zero eigen- values, associated with translations in two inde- pendent directions and the phase-shift symme- try; generically the remaining eigenvalues have nonzero real part. When the discrete symme- try is reduced from h, (or Dz ) to Z, the zero eigenvalues remain while the real parts of the other eigenvalues stay bounded away from zero provided the symmetry breaking from Z, (or Dz ) to Z, is sufficiently weak. Since the former is the limit of the rhombic lattice as 8 + 7r/2 while the latter is its limit for slow rotation rates it follows that Z, symmetric analogues of the SS and AR states persist on the rotating rhom- bic lattice and that one or both may be stable. On the other hand the SCR states (32) are saddles in the associated spherical system (26) when (n,h) = (m,e) [16]; we expect them to remain unstable for coefficient values close to

(n,h) = (m,e).

5. Heteroclinic cycles and quasiperiodic standing waves

In this section, we focus on instabilities of the TR and SR solutions in the TB and SB subspaces, respectively. We determine conditions for the formation of various types of heteroclinic orbits connecting either the two travelling rolls states or the two standing rolls states. We associate the formation of such heteroclinic orbits with the onset of a Kiippers-Lortz-like instability for os- cillatory rotating convection.

We begin by recalling that if the TR and SR solutions both bifurcate supercritically, then within the MR subspace one of them is stable while the other is unstable. We consider first the case where the TR are supercritical (a, < 0) and stable with respect to counterpropagating

perturbations: br - a, < 0. In order to under- stand the origin of the Kiippers-Lortz (here- after KL) instability for travelling rolls, we con- sider the case where the TR states are stable for small enough rotation rates. Increasing the rotation rate can then trigger the KL instability in one of four ways, associated with the four ways that the quasiperiodic TBi or TBz solu- tions may cease to exist as (c, - a,) (fr - a,) or (dr - a,) (g, - a,) change from positive to neg- ative. To see this consider the dynamics in the TBi subspace when (cr -a,) (fr -a,) < 0. Writ- ing z = (ri eibl,r2 e’@2,0,0) in equation (13) one finds that the amplitude dynamics (ii, i3 )

decouple from the phase dynamics ($1, $2 ), and

ii = (A + a,$ + c,r,2)r*

r5 = (1 + a,$ + frrflr2 . (39)

The TRi solution satisfies (ri, r2) = (r, 0) and the TRz solution satisfies ( rI, t-2 ) = (0, r), r2 = -A/u,. A sufficient condition for trajectories to remain bounded in the ( rl , r2 ) plane is cr + fr + 2u, < 0, in which case there is a saddle-sink heteroclinic orbit between TRi and TRz in the (rl , r2 ) plane [ 17 1. If fr - a, > 0 then the orbit originates at TRi and terminates at TRz in the TBi subspace. In this case the KL instability is in the counterclockwise or prograde direction. If instead c, -a, > 0 then TRz lose stability to TRi in the TBi subspace and the KL instability is in the clockwise or retrograde direction. Alterna- tively, the KL instability may occur in the TBz subspacewhen (d,-u,)(g,-a,) < O.Ifd,-a, > 0 then the instability is from TRz to TRi in the prograde direction, whereas if g, - a, > 0 then the KL instability is in the opposite direction. In all of these cases the instability is completely analogous to the KL instability for steady rolls (see section 1) . As in the steady case once a TR loses stability to another TR at an angle 8 to it- self the new pattern is again unstable to like per- turbations at the same angle 8 to itself, and so on. Note that as for the KL instability of steady

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226 E. Knobloch, M. Silber / Oscillatory convection in a rotating layer

rolls the KL instability of travelling rolls is as- sociated with the disappearance of an unstable pattern - in this case a TB pattern.

An interesting situation arises when both TR solutions are stable in the MR subspaces (b, < a, < 0), but unstable in the full space ( (fr - a,)(g, - a,) < 0, (c, - a,)(d, - a,) < 0). This situation may occur at fixed 8 for rotation rates larger than the critical rotation rate where the KL instability first appears. In this case, we ex- pect a continuous band of angles 8 for which TR are KL unstable. The heteroclinic cycle we now describe will be present provided the band includes angles 8 and n - 8 (e.g., 8 z 7r/2). Note first that the absence of the quasiperiodic travelling bimodal solution in the TBi subspace ( (fr - a,) (c, - a,) < 0) now implies the absence of the quasiperiodic TBz solution as well ( (d, - a,)(gr - a,) < 0). In this case when fr - a, > 0 there is a structurally stable heteroclinic orbit connecting TRi to TR2 in the TBr subspace at the mme time as there is a similar orbit con- necting TRz to TRi in the TB;! subspace, pro- vided the trajectories remain bounded in both subspaces. By applying the discrete symmetries of the rhombic lattice it is easy to see that un- der these conditions the above heteroclinic or- bits are in fact parts of a structurally stable hete- roclinic cycle connecting, in a counterclockwise fashion, four sets of rolls travelling in different directions (see fig. 5 ). The structural stability of the cycle, which is composed of saddle-saddle connections in the full eight-dimensional space, is a consequence of the symmetries that guaran- tee the existence of the invariant fixed point sub- spaces [ 181. Sufficient conditions for the exis- tence of such a heteroclinic cycle are

G + .L + 2G < 0, dr + g, + 2ar < 0; (40)

.L - a, > 0, gr - a, < 0,

c, - a, < 0, d, - a, > 0, (41)

where conditions (40) guarantee that trajecto-

TR; TR; j-,0.0,0) 10,~,0,0)

Fig. 5. The structurally stable attracting heteroclinic cycle shown in fig. 6 connects four travelling roll solutions as shown above. The TR,, j = 1,2, state is labeled by its (z,, ~2, z3, z4) coordinates. The superscripts e and r indi- cate whether the rolls are left-travelling or right-travelling.

ries remain bounded in the TB subspaces. More- over, with the help of theorem 2.10 of Melbourne et al. [ 171 we can show that the following con- ditions suffice for the cycle to be asymptotically stable:

min(-24,4 - gr,fr - b,)

x min(-2u,, a, - c,, d, - b,)

> (fr - a,) (d, - a) > 0 > a,. (42)

Fig. 6 illustrates the approach to such a cycle. It is characterized by an abrupt cyclic switching between the four sets of travelling rolls, with the length of time it takes to complete the full cy- cle increasing each time around. Note that the heteroclinic cycle is traversed in the opposite di- rection if the inequalities (41) are all reversed (i.e., (fr, g,) +-+ (cr, d,)). The heteroclinic cycle described here generalizes the cycle present on the rotating square lattice [9]. However, in the square case the four travelling rolls are related by symmetry (rotations by n/2 ) and the formation of the four way heteroclinic cycle is inevitable whenever there is a KL instability for 8 = n/2.

The possibilities for a KL instability of stand- ing rolls are much richer. We take a, < -IbJ so that SR are supercritical and stable with respect to travelling roll perturbations. In this case, in- stabilities of the SR solutions are investigated

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E. Knobloch, M. Silber / Oscillatory convection in a rotating layer 221

0.:

bll

0.t

0.

1241

0.1

5

0 i_l 0

1

i 0.01 2000 4000 8000 0

t

L I I 0.c 2000 4Oco 6000 8000

2000 4000 6000 8OOfl

t

L

2000 4000 6000 8000

t

Fig. 6. Solution of equations (13) with p = 0.2 + i, a = -1 + i, b = -1.5 -i, c = -1.3, d = -0.8 - 0.5, e = 1.3 - 0.7i, f = -0.5, g = -1.9 + 0.3i, and h = -1.4 - 0.6i. Clockwise, the four panels show Izl (t)l, jzz(t)l, Iz3(t)l, and Iz4(t)l vs. t. The panels illustrate the approach to an attracting heteroclinic cycle from an arbitrarily chosen initial condition.

in the SB subspace. This is accomplished by ex- We now discuss the possible asymptotic dy- amining the dynamics on the sphere (26). To namics when one of the SR solutions is stable guarantee that the trajectories on S2 represent and the other is unstable in the SB subspace. bounded dynamics in R3, we require go (6, p) < Specifically, we assume that SR2 is the stable so- 0 in (24) for all 8, v, E [0, K]; a sufficient con- lution (02, > 0, lm12 > lej2). We restrict our dition for this inequality to hold is 4(a, + br) < discussion, for the time being, to the dynamics m, + nr - (ej - [III, where m and n are given by of the spherical system (26). There are two sub- (22). In this case, orbits of (24) are attracted to a two-dimensional invariant manifold in R3;

cases to consider: ( 1) SRi is a saddle (In I2 < lh12), (2) SRi is a source (nr < 0, ]nl2 > lh12).

(26) then represents a projection of the dynam- In the case where SRi is a saddle, we expect sub- ics onto the unit sphere [ 161. In this way, we maximal fixed points to exist in the spherical are guaranteed that fixed points, limit cycles system. If these are unstable and there are no and heteroclinic orbits in the two-dimensional limit cycles present in the spherical system, then, spherical system (26) represent the same types generically, the unstable manifold of SRi lies in of structures in the R3 system (24). Recall that the stable manifold of SR2 and we have a hete- a fixed point in the spherical system represents roclinic orbit from SRi to SR2. In the case where a periodic orbit in the SB subspace. Similarly, a SRr is a source, we can readily determine suffi- limit cycle in the spherical system corresponds cient conditions for the stable manifold of SR2 to a quasiperiodic solution of (2 1). to coincide with the unstable manifold of SRi

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228 E. Knobloch. M. Silber / Oscillatory convection in a rotating layer

in the spherical system. This is accomplished by demanding gi (6, v,) > 0 in (26) for all 8, ~1 E [ 0, n ] so that 19’ > 0 everywhere except at SR, and SR2 (i.e., at 8 = 0, n ). We observe that gi > 0 if m, > Jel and n, < --I/z/ (fig. 3a). In this case, there do not exist any quasiperiodic or submax- imal periodic solutions in the SB subspace, and SR2 is a global attractor in the SB subspace.

The possibilities for heteroclinic connections between SRi and SR2 described above were identified by Swift and Barany [ 111 in the spe- cial case of standing rolls on a hexagonal lattice. In this case, there are three sets of standing rolls (SRI, SR2, SRs), each with a different wave vector orientation. The rolls, related by 27c/3 rotations of the hexagonal lattice, have the same stability properties. Consequently, if there is a heteroclinic connection from SRi to SR2, then there is also one from SR2 to SRs and from SRs back again to SRI. Thus the onset of the KL in- stability for SR on the hexagonal lattice is asso- ciated with the formation of a heteroclinic cycle. Moreover, Swift and Barany showed that when the cycle consists of saddle-focus connections in the spherical system there is the possibility of chaotic dynamics of Shil’nikov type.

Finally, we point out that it is possible for SRi and SR2 to be the only fixed points in the spher- ical system and for both of them to be unsta- ble. The Poincare-Bendixson theorem [ 19 ] then guarantees the existence of a limit cycle in the spherical system; this corresponds to a quasiperi- odic standing wave solution of ( 13 ) . Sufficient conditions for a limit cycle to exist in the spher- ical system (26) are

mr < 0, n, < 0, Iml > le], InI > lhl; (43)

mi < +I, ni > IhI,

or mj > ]e], 12j < -I/z]. (44)

The inequalities (43) guarantee that SRI and SR;! are both sources in the spherical system. The inequalities (44) guarantee that p’ > 0 or

q” < 0, respectively, everywhere on the sphere. Thus the only fixed points on the sphere are at the north pole and the south pole (i.e., SR, and SR2). Since the dynamics are bounded on S2, and the only fixed points are sources at the poles, there must exist a limit cycle encircling the sphere. Fig. 7 shows the approach to such a quasiperiodic solution of ( 13). Note that the quasiperiodic standing bimodal pattern is not a relative equilibrium (i.e., it does not coincide with the group orbit of a point in c4). In this way it differs fundamentally from the quasiperiodic travelling bimodal patterns: there does not exist a co-moving frame in which the quasiperiodic SB solutions are singly-periodic. As with the TB states, the quasiperiodic SB solution may appear in a primary bifurcation. Furthermore, we note that the quasiperiodic SB solution may vanish in a Hopf bifurcation with, say, SR2 as m, is varied through 0 leaving in its wake a IU instability of SR, to SR2.

6. Discussion and conclusion

In this paper we have studied doubly-periodic patterns on the rotating rhombic lattice. We have shown that there are always four primary branches of (temporally) periodic states: these are the travelling and standing rolls in the two directions ki and k2. In addition we showed that in open regions in coefficient space there may be two or four additional primary branches of periodic solutions with submaximal isotropy; in particular these exist for a nearly square ro- tating lattice or for a rhombic lattice that rotates slowly. We also found two primary branches of two-frequency (quasiperiodic) travelling states in open regions in coefficient space. The exis- tence of an additional primary bifurcation, to a quasiperiodic standing wave pattern, was in- ferred using the PoincarbBendixson theorem. We have not, however, determined whether any nonsymmetric triply periodic solutions (QP3) exist as primary branches. Our results are closely related to existing results for the rotating square

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E. Knobloch, M. Silber / Oscillatory convection in a rotating layer 229

200 400 0 200 4(X)

(a) 1

W 1

Fig. 7. Solution of equations (13) with p = 0.1 + i, a = -1 + i, b = 0.3 - i, c = 1.3, d = -1.3 - 0.55, e = 0.4 + 0.2i, f = - 1 S, g = 1.1 + 0.2i, and h = 0.1 - 0. li showing approach to a quasiperiodic solution from an initial condition out of the SB subspace. (a) Oscillations in the amplitudes 11~ 1, 1231 vs. t. (For the periodic solutions the amplitudes are constant.) Note that after a short transient [ztl z 1~31. (b) Amplitudes 1~21 and 1241 vs. t.

lattice [9] and the nonrotating rhombic lattice [ lo]. We highlight here some of the key differ- ences.

On the rotating rhombic lattice there are two branches of travelling rolls and two of standing rolls, each with different stability properties. On the square lattice the TR branches are identified by an additional symmetry (rotation through 7r/2), as are the two SR branches. On the non- rotating rhombic lattice these solution branches are related by reflection symmetries. In both of these special cases the stability properties of the TR solutions are identical, as are the stability properties of the SR solutions. As discussed in section 3, there are two additional patterns with maximal isotropy on both the rotating square lattice and the nonrotating rhombic lattice: these correspond to primary branches of stand- ing squares (SS) (or standing rectangles in the rhombic case) and of alternating rolls (AR). On the rotating rhombic lattice these become stand- ing bimodal patterns with submaximal isotropy and are no longer always present. The two quasiperiodic travelling bimodal patterns on the rotating rhombic lattice are related by a 7r/2 rotation symmetry on the rotating square lattice and thus have the same branching and stability properties. On the nonrotating rhombic lattice, the two travelling bimodal solutions become sin-

gle frequency travelling rectangle patterns with maximal isotropy; the patterns travel along the two axes of reflection symmetry of the rectangle and do not have the same stability properties.

In the previous section we identified various types of Kuppers-Lortz instabilities for both travelling and standing rolls. We use this term to refer to instabilities of a roll pattern with respect to another pattern with a different orientation. These instabilities do not occur in nonrotating systems for which reflection symmetry precludes a preferred direction of instability. In the case of travelling rolls the instability is of precisely the same form as the well-known Kiippers-Lortz instability for steady rolls; in both cases the in- stability is triggered by the disappearance of an unstable pattern and the formation of a hetero- clinic orbit. Under appropriate conditions we found, in addition, a structurally stable hetero- clinic cycle connecting rolls travelling in four different directions. This cycle is the direct ana- logue of the structurally stable heteroclinic cycle whose formation triggers the KL instability of travelling rolls on the rotating square lattice. On the rotating rhombic lattice the cycle exists if the fluid rotates rapidly enough for such an in- stability to be present in a band containing both 8 and K - 8, where 8 is the angle between ki and k2. While this cycle may be asymptotically

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230 E. Knobloch. M. Silber / Oscillatory convection in a rotating layer

stable when the solution space is restricted to patterns periodic on the rhombic lattice, it is not attracting in the infinite-dimensional hydrody- namic problem. This is because each TR solu- tion is unstable to a continuum of TR oriented at all angles 8 within the KL unstable band. The resulting dynamics in the infinite-dimensional case may be quite complicated.

For travelling rolls we found that whether or not a KL instability occurs is largely determined by the linear stability of the TR states. This is not the case for SR solutions. We did not derive a simple criterion, in terms of the coefficients of the normal form equations, for existence of a IU instability for SR. The difficulty arises in trying to rule out the possible coexistence of quasiperi- odic or submaximal periodic attractors in the SB subspace with a stable SR solution when the other SR state is unstable. We were able to do this only in a particular case where one of the SR solutions was a sink and the other a source in the associated spherical system. In this case we could identify the origin of the ISL instability with the disappearance of a quasiperiodic stand- ing wave solution.

Thus far we have focused attention on the gen- eral rhombic lattice, and treated the square lat- tice as a special case. The square lattice has the property that a KL instability of travelling rolls guarantees the existence of a heteroclinic cycle connecting the four TR states. This is because the four competing TR patterns are related by symmetry (rotation by n/2 ). In contrast, the ob- servation that the two orthogonal SR patterns must have the same stability properties may be used to prove that there cannot be a ISL instabil- ity for SR at 8 = n/2. Specifically, on the rotat- ing square lattice the only possibility for a het- eroclinic connection between the two SR solu- tions is via a structurally unstable saddle-saddle connection in the spherical system (26). Thus there is no KL instability of standing rolls on the square lattice. There is one other doubly- periodic lattice that has the property that the SR and TR states are related by a rotational symme-

try of the lattice. This is the hexagonal case, stud- ied extensively in the nonrotating case for both steady state [ 13 ] and Hopf bifurcations [ 201. It has also been analyzed for steady state bifurca- tions in the rotating case [ 151. Some aspects of the dynamics on the hexagonal lattice follow as special cases of the analysis presented above for the rhombic lattice. We deduce these below but make no attempt to provide a complete discus- sion of this problem. We begin by observing that the stability of TR and SR on the hexagonal lat- tice may be determined by considering the spe- cial case of the rhombic lattice with 8 = n/3. We let I, = Z, x T2 x S’ denote the symmetry group associated with the hexagonal lattice. In this case there are three left-travelling rolls in the k i, k2, k3 directions with amplitudes zI, ~2, z3 E @, and three right-travelling rolls with ampli- tudeswr,w2,ws E C.Herewetake]kl] = lk21 = lk31 = kc and kl + k2 + k3 = 0. The action of Ih on C6 is generated by

P: (~1,~2,~3;~I,~2,~3)

+ (z2, z3, zl; w2, w3, WI ),

K: (zl,z2,z3;w1,w2,w3)

+ (~1,~2,~3;~1,~2,~3),

+ ( ei& z,, e-i(h+02) ~2, e

iO2 ~3;

e --if4 w,, eitOb+e2)

~2, e -io2 Wj),

4: (~1,~2,~3;~1,~2,~3)

(45)

where p,~ E Z,, (O,,&) E T2 and 4 E S’. The two rhombic subspaces containing the SRI so- lution are RH1: (zl, z2,0;w1,w2,0) and RH2: (z1,0,z3;w1,0,w3). These are related by the rotational symmetry p E z6. Thus we focus on the invariant subspace with z3 = w3 = 0 (8 = n/3 ), which is fixed by the group element [(7c,O),n] E T2 x S I. We note that the group

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E. Knobloch. M. Silber / Oscillatory convection in a rotating layer 231

elements of rk act on points in the rhombic sub- spaces in precisely the same manner as T acts on UZ4. Thus, the Ii,-equivariant vector field, restricted to RHi is I-equivariant. That this restriction yields a generic T-equivariant vector field may be verified for the cubic truncation of the general Ii,-equivariant vector field [ 111:

ii = 21 (p + a]z,]* + b]W,]* + c,lz212

+ 41w212 + ~21Z312 + &lw12)

+ ml (el z2w2 + e2z3w3 ), (46)

where the remaining components of the vector field are generated by letting Z, act on ii and the coefficients /L, a, b, cj, dj, ej (j = 1, 2) are all complex. The stability of TR and SR on the hexagonal lattice may be determined by cal- culating the stability of TRj, SRj (j = 1, 2) in the rhombic subspace RHi. For SR there are four eigenvalues, two of which are zero, in the MR subspace (z i , 0,O; w 1, 0,O). The remaining eight eigenvalues are associated with the SB sub- space of RH 1: two eigenvalues, each of multiplic- ity two, for each of SRi and SR2. For TR there are also four eigenvalues associated with the MR subspace: one is zero, one is associated with the branching direction and two come as a complex conjugate pair. The remaining eight eigenvalues are associated with the TBi and TB2 subspaces of RH 1: two complex conjugate pairs for each of TRi and TR2. Note that on the hexagonal lat- tice the six left- and right-travelling rolls in the directions kj (j = 1, 2, 3) are related by sym- metry as are the three standing rolls. Thus they must all have the same stability properties.

Although the calculations described in this pa- per are completely general they are motivated by convection in a plane layer rotating about the vertical. It was shown by Chandrasekhar [ 41 that in such a layer convection sets in as over- stable oscillations for sufficiently small Prandtl numbers Pr. When the centrifugal force is small relative to gravity the rotation affects the sys- tem through the Coriolis force only, and the re-

sulting equations for an unbounded layer are translation-invariant. With the assumptions dis- cussed in section 1 the governing Navier-Stokes equations can be reduced to the normal form (6) if the onset of convection is steady or to the nor- mal form ( 13) if it is oscillatory. In the former case the KL instability is triggered when c-a be- comes positive. For large Pr this first occurs for an angle 8 near 59” and the resulting instability is in the direction of rotation [ 3,5]. For the os- cillatory instability states only partial results are available. Knobloch and Silber [ 2 1 ] showed that with stress-free and fixed temperature boundary conditions at the top and bottom TR were pre- ferred over SR in the range 0.53 < Pr < 0.68 with SR preferred for small rotation rates and TR preferred for large rotation rates when Pr < 0.53. Qualitatively similar results hold also for rigid boundaries [ 221. However, in these papers the stability properties of these states with re- spect to perturbations oriented at some angle 19 were not investigated. More recently, Riahi [ 23 ] has considered the stability properties of stand- ing patterns with stress-free boundary conditions with respect to perturbations in various direc- tions. He finds that standing rolls are always su- percritical and always unstable with respect to such perturbations (provided 8 # a/2 for rea- sons explained above). Riahi thus shows that the standing rolls that are stable with respect to trav- elling roll perturbations with 8 = 0 are always unstable in the SB subspaces. However, the dy- namics in the SB subspace was not determined. In particular, Riahi did not consider standing wave patterns in which the two sets of standing rolls were phase shifted, in time, relative to each other. We are thus unable to determine from Riahi’s calculation whether the instability of the standing rolls is in fact a Kiippers-Lortz type of instability. However, even if this is the case, it is likely to be a consequence of the stress-free boundary conditions used; with these boundary conditions steady rolls are also always KL unsta- ble [ 241. The techniques used in this paper clar- ify the mechanism for KL-like instabilities, and

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232 E. Knobloch. M. Silber / Oscillatory convection in a rotating layer

in addition specify precisely the calculations that must be performed to establish their existence. We hope that this paper will spur efforts in this direction.

Acknowledgements

This work was presented at a conference on Bi- furcation and Symmetry, held in Marburg, Ger- many, in June 1991. We have benefited from discussions with Ian Melbourne and Jim Swift. The work of E.K. was supported in part by NSF grant DMS-88 14702 as well as an INCOR grant through the Center for Nonlinear Science at Los Alamos National Laboratory.

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