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Proceedings. Mathematical, Physical, and Engineering Sciences logoLink to Proceedings. Mathematical, Physical, and Engineering Sciences
. 2014 Aug 8;470(2168):20140093. doi: 10.1098/rspa.2014.0093

Inertial modes in a rotating triaxial ellipsoid

S Vantieghem 1,
PMCID: PMC4075787  PMID: 25104908

Abstract

In this work, we present an algorithm that enables computation of inertial modes and their corresponding frequencies in a rotating triaxial ellipsoid. The method consists of projecting the inertial mode equation onto finite-dimensional bases of polynomial vector fields. It is shown that this leads to a well-posed eigenvalue problem, and hence, that eigenmodes are of polynomial form. Furthermore, these results shed new light onto the question whether the eigenmodes form a complete basis, i.e. whether any arbitrary velocity field can be expanded in a sum of inertial modes. Finally, we prove that two intriguing integral properties of inertial modes in rotating spheres and spheroids also extend to triaxial ellipsoids.

Keywords: rotating flows, inertial modes, triaxial ellipsoid

1. Introduction

One of the most striking features of incompressible, rotating flows is their ability to sustain wave motion. The restoring force giving birth to these waves is the Coriolis force. Because this phenomenon only relies on inertia, eigenmodes of wave propagation in bounded geometries bear the name inertial modes. Numerous studies, both computational and experimental, have shown that these waves can be excited and maintained in different ways, e.g. by thermal and shear instabilities [1,2], libration [3], precession [46], tides [7] or differential rotation [8,9].

The Coriolis force being dominant in the force balance that governs the dynamics of numerous geo- and astrophysical bodies, it is widely believed that inertial modes are fundamental concepts for our understanding of many of these bodies' properties. For instance, inertial modes emanate at the onset of small Prandtl number convection in a rapidly rotating sphere subjected to volumetric heating [1], as is the case in astrophysics. Furthermore, several authors have argued that the ancient lunar dynamo [10] and Io's magnetic signature [11] are generated by complex fluid motions that arise as a result of a so-called elliptic instability. This phenomenon can be understood as the resonant coupling between two inertial modes and a strain field due to the tidal deformation of the celestial body under consideration [12].

To verify and clarify these mechanisms, a number of studies have been devoted to the dynamic response of fluid-filled rotating triaxial ellipsoids to harmonic forcings, such as libration [1315], precession [16] and tides [17]. However, neither laboratory experiments nor numerical simulations can reach the extremely low values of viscosity that characterizes the dynamics of planetary cores. The strength of viscous effects is usually quantified by means of the Ekman number, a non-dimensional estimate of the ratio between the viscous force and the Coriolis force. In planetary settings, the value of the Ekman number typically takes values in the range 10−15–10−10. For the laboratory experiments cited, this quantity has order-of-magnitude 10−6–10−4. Numerical studies even have to compromise further on the value of the Ekman number. To compensate for this discrepancy, the aforementioned studies have been carried out in enclosures whose ellipticity is much larger than that is encountered on a geo- and astrophysical scale. However, existing theories are built upon the assumption that the equatorial deformation is small such that the mathematical analysis can be pursued in terms of spheroidal inertial modes [17,18]. To bridge the gap between theory on the one hand, and simulations and experiments on the other hand, it would be convenient to deduce an analytical expression for inertial modes in triaxial ellipsoidal geometry. This is the context in which this work was conceived. Apart from this, the problem of inertial modes in a rotating triaxial ellipsoid is also an interesting mathematical question in its own right.

Pioneering work regarding the theory of inertial modes was established by Kelvin [19], who derived an expression for inertial oscillations in a cylindrical geometry. Shortly afterwards, Poincaré [20] formulated the generic mathematical theory describing such oscillations. Bryan [21] on the other hand provided a general implicit expression for the inertial modes in a spheroidal geometry. Note that we use the terminology ‘spheroid’ to signify an ellipsoid whose two axis perpendicular to the rotation axis are equal. These theories were rediscovered independently by Bjerknes and co-workers [22], who termed them ‘elastoid-inertia’ oscillations. Later contributions have focused on the effect of the presence of a finite but small amount of viscosity. A major tour de force in this context is the expression for the corrective boundary layer in a spherical and a spheroidal geometry [2325]. In the same era, Kudlick also proposed a procedure to calculate explicitly spheroidal inertial modes; this however involves finding the roots of a polynomial of high-degree, and thus requires numerical work. More recently, Kerswell [16] showed that spheroidal inertial modes could be constructed from finite-dimensional bases of polynomial vector fields. Zhang and co-workers, on the other hand, were the first ones to obtain explicit expressions for all possible inertial modes that can exist in a spherical and spheroidal geometry [26,27]. Furthermore, much attention has been devoted to non-smooth inertial wave solutions that can be excited in a spherical shell [2830] or parallelepiped [31]; in the low-viscosity limit, these take the form of wave attractors.

This work builds upon and extends the existing theories of inertial modes in the following sense: (i) we outline a procedure to compute inviscid inertial modes in a triaxial ellipsoid. We apply this technique to compute, for the first time, a handful of eigenvalues and eigenmodes in triaxial geometry. In this sense, our contribution is somewhat similar to the results obtained by Kudlick [25] for inertial modes in a spheroid. It is also an extension of the approach of Kerswell [16] to triaxial ellipsoids. Furthermore, following Greenspan [32], an expression for the viscous corrections to the eigenvalue is at hand, once the inviscid problem has been solved. In this work, we will compute these corrections for one particular class of modes. (ii) We shed new light on the still open question whether the inertial modes form a complete set, i.e. whether it is possible to expand an arbitrary, sufficiently smooth solenoidal vector field in a series of inertial modes. (iii) We prove that two integral properties of inertial modes, originally discovered by Zhang et al. [27,33] for rotating spheres, extend to triaxial ellipsoids.

2. Mathematical formulation

We consider an inviscid and incompressible fluid contained within a triaxial ellipsoid of semi-major axes a, b and c. In mathematical terms, it is described by

x2a2+y2b2+z2c2=1. 2.1

The notations x,y,z refer to the cartesian coordinates. In the following, we will denote the position vector as r, i.e. r=(x,y,z). The ellipsoid is rotating at angular speed Ω0 around the z-axis. We now consider the equations of mass and momentum conservation for small amplitude motion of an inviscid compressible fluid, expressed within a frame of reference rotating with the ellipsoid

U=0 2.2

and

Uτ+2z^×U+P=0. 2.3

Here, τ denotes time with respect to the time scale Ω01, z^ is the unit vector along the rotation axis, and U and P are the velocity and pressure field. We have dropped the nonlinear term in the momentum equation (2.3), as we assume small amplitude motion. Inviscid inertial modes are then solutions of (2.2) and (2.3) of the form U=u(r)exp(iλτ), P=p(r)exp(iλτ). The scalar λ is termed the eigenvalue or eigenfrequency, and the fields {u,p}eigenmodes. As such, the above equations can be reformulated as follows:

u=0 2.4

and

2z^×u+p=iλu. 2.5

Finally, the system of equations (2.2) and (2.3) or (2.4) and (2.5) should be supplemented with the non-penetration condition at the boundary of the ellipsoidal volume

Un^=un^=0, 2.6

where the vector n^ denotes the unit outward normal to the triaxial ellipsoid:

Equation (2.5) can be recast in terms of the vorticity ω≡∇×u.

×(2z^×u)=iλω. 2.7

We note that the non-penetration condition (2.6) does not impose any constraint on the vorticity field.

It can be shown that the eigenvalues λ are real and −2≤λ≤2 [32]. Furthermore, eigenmodes u satisfy the following orthogonality relationship:

uiujdV=δij, 2.8

provided that λi≠λj. The notations † and δij, respectively, refer to the complex conjugate and the Kronecker delta. In this expression, and in the remainder of this article, the integration domain for three-dimensional integrals is always the ellipsoidal volume bounded by (2.1).

3. An algorithm to find inertial modes

In this section, we will develop a method to compute inviscid inertial modes in a triaxial ellipsoid. Most authors who have addressed this problem in other geometries, did so by recasting the eigenvalue problem (2.4)–(2.6) in terms of the pressure alone. This yields the famous Poincaré equation [20]

2p(λ2)2(z^)2p=0, 3.1

supplied with the boundary condition

(z^p)(z^n^)(λ2)2n^piλ2(n^×z^)p=0. 3.2

For −2≤λ≤2, this equation is hyperbolic and is in general ill-posed; this implies that it has singular solutions that are not square-integrable [28,34]. However, for specific geometries, such as cylinders, spheres and spheroids [21,25], and annular ducts [35], the problem is well posed and regular solutions for the pressure eigenmodes can be constructed. Once these are found, an expression for the velocity eigenmodes is at hand.

Although it is possible to separate the Poincaré equation for rotating triaxial ellipsoids in terms of ellipsoidal coordinates [36], we will adopt a different approach here. We will start from the hypothesis that the inertial modes {u,p,ω} can be written as polynomials in terms of cartesian coordinates x, y and z. There are multiple motivations for this ansatz. First, it is well known that inertial modes in spheres and spheroids [21,23,25] are of this form. Furthermore, polynomial solutions of the Poincaré equation in triaxial ellipsoids have been studied previously, among others by Cartan [37] and Lyttleton [36]. Finally, investigations of the linear stability of flows within rotating triaxial ellipsoids [3841] suggest that the Coriolis operator is closed within certain subspaces of polynomial velocity fields.

This section is now organized as follows. In §3a, we present the concept of vector spaces of solenoidal polynomial vector fields. This will allow us, in §3b, to reformulate the problem (2.4)–(2.6) as a finite-dimensional eigenvalue problem for which a full spectral decomposition is granted. In §3c, we will then apply this approach by computing eigenvalues and eigenmodes for subspaces of low polynomial degree. In §3d, we will address the first-order viscous corrections of the eigenfrequencies. Finally, §3e is devoted to a comparison between theoretical results and numerical simulations.

(a). Preliminary concepts

In the following, we present concepts regarding vector spaces of polynomial vector fields in ellipsoidal domains. This theory was originally devised by Gledzer and Ponomarev [38] and Lebovitz [42], and was also thoroughly covered in a recent work by Wu & Roberts [40] (see their appendix A). It can be described in terms of two vector spaces that we will denote Wn and Vn. These are defined as follows: Wn is the vector space of solenoidal vector fields w whose cartesian components are homogeneous polynomials of degree n in the cartesian coordinates. Vn is the vector space of solenoidal vector fields v that satisfy (2.6), and are such that ×vWn. These vector spaces have the following properties:

  • (i) If we consider a toroidal–poloidal decomposition of an element w of Wn
    w=×t(r)r+××s(r)r, 3.3
    then it is always possible to write t as a homogeneous polynomial of degree n and s as a homogeneous polynomial of degree n+1. Furthermore, adopting spherical coordinates (r,θ,ϕ), we can use the fact that the spherical harmonics Ylm(θ,ϕ) of degree l and order m have a polynomial representation [43]. This allows the finding of an expansion for t and s of the following form:
    t=rnl=1mod(l,n)=0ntlmYlm(θ,ϕ) 3.4
    and
    s=rn+1l=1mod(l,n)=1n+1slmYlm(θ,ϕ). 3.5
    To generate a basis for Wn, one can simply take the vector fields that are associated with each individual spherical harmonic Ylm in (3.4) and in (3.5).
  • (ii) The vector spaces Wn and Vn are isomorf, i.e. for any given element w of Wn, one can find exactly one solenoidal vector field v such that w=∇×v and v satisfies the no-penetration condition (2.6). As such, we can introduce the ‘inverse curl operator’ ∇−1× that acts on elements of Wn and generates elements of Vn. We will write this as
    v=1×w. 3.6
  • (iii) The elements of Vn are polynomials of degree n+1 in the cartesian coordinates.

  • (iv) The dimension of Wn and Vn is (n+1)(n+3). [42]

For further corroborations, including a more rigorous mathematical underpinning of some of these properties, we refer to appendix A.

We also introduce the vector spaces W~n and V~n. Here, W~n is the vector space of all solenoidal vector fields w whose cartesian components are polynomials (not necessarily homogeneous) of maximum degree n, i.e.

W~nWnWn1Wn2 3.7

The vector space V~n is defined likewise, i.e.

V~nVnVn1Vn2 3.8

In the following, we will denote the dimension of V~n and W~n as N.

(b). The inertial mode equation projected onto V~n and W~n

We now return to the inertial mode problem, and look for velocity eigenmodes u that are restricted to V~n; its corresponding vorticity eigenmode ω belongs to W~n. We use (3.6) to ‘uncurl’ expression (2.7) as follows:

1××(2z^×u)=iλ1×ω, 3.9
=iλu. 3.10

Now, we note that the operation

×(2z^×u)=2zu 3.11

transforms uV~n into elements of W~n. Indeed, the polynomial degree of u being part of V~n is not higher than n+1; thus, (∂/∂z)u is of maximum polynomial degree n. Moreover, (∂/∂z)u is solenoidal given that u also satisfies this property. From these two arguments, it follows that ×(2z^×u)W~n. This implies that the left-hand side of (3.10) defines a linear operator L on V~n. We can recast (3.10) as follows:

Lu=iλu, 3.12

Furthermore, we endow the vector space V~n with an inner product that we denote as 〈vjvk〉 and is defined as follows:

vj,vk=vjvkdV. 3.13

Once this is established, it is possible to generate an orthonormal basis {e1,e2…,eN} for V~n. As such, any element u of Vn can uniquely be decomposed as

u=k=1Nγkek, 3.14

with γk=〈u,ek〉.

Of utmost importance now is that the operator L is skew-Hermitian, i.e.

vj,Lvk=Lvj,vk. 3.15

The proof of this is straightforward. Indeed, one has

×Lvk=×(2z^×vk) 3.16

and thus

Lvk=2z^×vkψ. 3.17

Given the solenoidal character of vj and the non-penetration condition (2.6), it follows that:

vj,Lvk=vj(2z^×vkψ)dV=vj(2z^×vk)dV. 3.18

In a similar way, one obtains

Lvj,vk=vk(2z^×vj)dV=vj(2z^×vk)dV. 3.19

Comparing (3.18) and (3.19), one finds indeed that (3.15) holds.

Using expansion (5.7), the eigenvalue problem (3.12) can be recast as

iλγk=l=1Nek,Lelγl. 3.20

The coefficients ek, Lel define the matrix elements Mkl of a square matrix M of finite size that is skew-Hermitian. Although the technique of polynomial vector spaces has been used before to find inertial modes in spheroidal geometry [16], we are the first to substantiate that the ‘inertial mode operator’ can be brought in skew-Hermitian form when projected onto these vector spaces. This is important because, by virtue of the spectral theorem, it ensures the following: (i) The eigenvalues of L (or M) are purely imaginary (i.e. λ is real) and whether are zero, or come in pairs ±iλk. (ii) It is possible to find N linearly independent eigenvectors that are solution of the inertial mode equation. Moreover, they are mutually orthogonal with respect to the inner product (3.13). In other words, the eigenvectors form an orthogonal basis for V~n. These properties hold for any n. As such, it is in principle possible to construct an arbitrarily large set of eigenmodes by using the procedure described above.

(c). Linear and quadratic inertial modes

In this section, we use the approach outlined in §3a,b to solve the inertial mode problem within the subspaces V~0 and V~1, i.e. for eigenmodes that are linear, respectively, quadratic polynomials in the cartesian coordinates. We will only discuss the final result here. For more details on the intermediate steps leading to these results, we refer to appendix B.

For the three-dimensional subspace V~0=V0, we find the following eigenvalues:

λ1,2=±2aba2+c2b2+c2andλ3=0. 3.21

We can rewrite λ1,2 in function of two independent, dimensionless parameters c¯ and β. To this end, we first introduce R, the mean equatorial radius

R=a2+b22. 3.22

This allows to define the dimensionless aspect ratio c¯ and ellipticity β

c¯=cRandβ=a2b2a2+b2. 3.23

As such, we can rewrite λ1,2 as follows:

λ1,2=±21β2(1+c¯2+β)(1+c¯2β). 3.24

In figure 1, we display contours of |λ1,2| in the (β,c¯)-plane. The velocity eigenmodes corresponding to these eigenvalues are

u1,2=(zc2x^xa2z^)ibaa2+c2b2+c2(zc2y^yb2z^)andu3=yb2x^+xa2y^. 3.25

All three eigenmodes are of uniform vorticity. For u1,2 the vorticity is purely equatorial; these eigenmodes are usually referred to as the spin-over mode. If we choose β=0, we obtain the classical result [25,27,41]

λ1,2=±2c¯2+1andu1,2=zc2(x^iy^)(xiy)z^. 3.26

for the spin-over mode and its eigenfrequency in spheroidal geometry.

Figure 1.

Figure 1.

Isocontours of |λ1,2|, the eigenfrequency of the spin-over mode given by expression (3.24), plotted in the (β,c¯)-plane. (Online version in colour.)

We now turn our attention to V~1. Since V~0 is a subspace V~1, the solutions (3.21)–(3.25) are also eigensolutions of the inertial mode problem for V~1. The eight other eigenvalues are associated with eigenmodes that are quadratic polynomials. These eigenvalues are the roots of the following characteristic polynomial, which is, for brevity, written in function of A=a2/c2,B=b2/c2:

(AB+A+B)[3(A+B)+AB+8][3(A+1)B+A+8B2][3(B+1)A+B+8A2]λ8+16AB[453A2B2+214A2B2(A+B)+213AB(A2+B2)+262AB(A+B)+52AB(A3+B3)+11(A2+B2)+26AB+55A3B3+26(A4+B4)+62(A3+B3)+18A2B2(A2+B2)]λ6+32A2B2[36AB(A2+B2)+52(A3+B3)+59(A2+B2)+12(A+B)+176AB+220AB(A+B)+111A2B2]λ4+256A3B3[6(A2+B2)+19AB+2(A+B)+1]λ2+256A4B4. 3.27

The zeroes of this polynomial come in four pairs ±iλj ( j=1,…,4). In principle, one can still find an explicit expression for λj. These are lengthy and cumbersome, and therefore, are not written here. However, for the spheroidal case (i.e. with β=0), the expression is more compact. We find

λ1=±10+49+c¯211+4c¯2,λ2=±1049+c¯211+4c¯2,λ3=±21+4c¯2andλ4=±21+2c¯2, 3.28

a result that was previously obtained by Kerswell [16], who used the same technique as the present one for a spheroidal geometry.

In figure 2, we show curves of constant |λj| in the (c¯,β)-plane. The isocontours are symmetric with respect to the axis β=0, which reflects the fact that the problem is invariant under an exchange of a and b. In figure 3, we illustrate the spatial structures of these modes. To do so, we provide meridional circulation patterns of the eigenmodes in the planes x=0 and y=0 for one specific geometry, defined by β=0.867,c¯=0.911. The four values of |λ| corresponding to subfigures a, b, c and d are, respectively, 1.078, 0.09572, 0.5796 and 0.3781. One of the more striking features is that the circulation pattern shown in subfigure (b) is virtually independent from z. Such an almost geostrophic profile is indeed consistent with a low value of λ=0.09572. As a further illustration, we also show these patterns for two selected eigenmodes of the vector space V~2, i.e. of polynomials of degree 3, in figure 4.

Figure 2.

Figure 2.

(ad) Isocontours of the absolute value |λj| of the eigenfrequencies of quadratic inertial modes within the subspace V~1, plotted within the (β,c¯)-plane. Each subfigure corresponds to one pair of roots ±iλj of (3.27). Corresponding circulation patterns of eigenmodes associated with these eigenvalue pairs can be found in figure 3. We note that λ1 in (3.28) corresponds to figure (a), λ2 to figure (b), etc. (Online version in colour.)

Figure 3.

Figure 3.

(ad) Meridional circulation patterns of quadratic inertial modes in the planes x=0 and y=0 for an ellipsoid defined by β=0.867 and c¯=0.911). Corresponding eigenvalues associated with these eigenmodes can be found in figure 2. (Online version in colour.)

Figure 4.

Figure 4.

(a,b) Meridional circulation patterns of selected cubic inertial modes of V~2 in the planes x=0 and y=0 for an ellipsoid defined by β=0.867 and c¯=0.911). (Online version in colour.)

(d). Viscous corrections of the spin-over mode frequency

In this section, we are concerned with inertial modes in a viscous fluid. Instead of (2.5), the governing momentum equation now reads

2z^×u+pE2u=iλu, 3.29

and the boundary condition (2.6) is replaced by

u=0. 3.30

The parameter E is termed the Ekman number, and obeys the following definition:

E=νΩ0R2. 3.31

Here ν denotes the kinematic viscosity, which is assumed uniform, and R is defined by (3.22).

The classical approach to the viscous problem is the one of asymptotic boundary layer theory [23,25,27,32]. For sufficiently small Ekman number, one assumes that the viscous eigenmode can be expanded as the sum of the inviscid eigenmode, and a number of corrections that are asymptotically small in their magnitude and/or spatial extent. More specifically, the velocity field can be decomposed in an interior flow uI and a viscous Ekman boundary layer uB that allows to accommodate the no-slip condition (3.30); the wall-normal thickness of this boundary layer is of order-of-magnitude E1/2. Each of these contributions, as well as the pressure and eigenfrequency, can then be expanded in a powers series in the Ekman number:

uI=uI0+E1/2uI1+, 3.32
uB=uB0+E1/2uB1+, 3.33
pI=pI0+E1/2pI1+ 3.34
andλ=λ0iE1/2G+, 3.35

In these expressions, the leading-order terms uI0,pI0 and λ0 denote the velocity, pressure field and eigenvalue of the corresponding inviscid mode. In general, G is a complex number, i.e. G has both a real and imaginary part, that correspond, respectively, to a viscous decay rate and frequency shift.

In this work, we are not concerned with solving the structure of the boundary layer flow uB or secondary interior flow u1. However, following Greenspan [32], §2.9, we can determine G, merely based on the inviscid frequency and velocity eigenmode profile. Indeed, G is given by

G=ISuI0uI0dV, 3.36

with IS the surface integral over the surface of the ellipsoid

IS=123/211(z^n^)2{|n^z^×uI0iz^uI0|2|b+|1/2(1+ib+|b+|)+|n^z^×uI0+iz^uI0|2|b|1/2(1+ib|b|)}dS, 3.37

and b±=λ0±z^n^. Although integral (3.37) can in general not be computed analytically, IS and G are readily evaluated numerically. As an illustration, we compute G for the spin-over mode. In figure 5, we show isocontours of the real and imaginary part of G in the (β,c¯)-plane. We find that the real part of G increases in absolute value with decreasing c¯ and increasing |β|. The imaginary part on the other hand also reaches its minimum for β=0. Furthermore, we can validate our results by comparing against the expressions for G for oblate spheroidal geometries (i.e. for β=0) derived by Zhang and co-workers [27]. Defining the eccentricity E=1c¯2, these authors provide the following asymptotic formulae for the real and imaginary part of G:

R(G)=3(19+93)282+1039+171312322E2+O(E4)=2.6200.4263E2+O(E4) 3.38

and

I(G)=3(19+93)282+1039+171312322E2+O(E4)=0.2585+0.7663E2+O(E4). 3.39

In table 1, we compare values of G obtained by numerical evaluation of the expressions (3.36) and (3.37) against their asymptotic counterparts (3.38) and (3.39). We find that the agreement between both values is within 1% for all values of E considered. However, we observe notable discrepancies for the imaginary part for E0.3. A MATLAB script that allows to compute G for a given β and c¯ is provided as the electronic supplementary material.

Figure 5.

Figure 5.

Isocontours in the (β,c¯)-plane of the real (a) and imaginary (b) part of the viscous correction G of spin-over mode eigenfrequency (for the positive value of λ1,2 in (3.21)). (Online version in colour.)

Table 1.

Comparison between numerically obtained and asymptotic values for G for oblate spheroidal geometries.

c¯ E G(from (3.36)–(3.37)) G(from (3.38)–(3.39))[27]
1 0 −2.620+0.2585i −2.620+0.2585i
0.99 0.14107 −2.629+0.2739i −2.629+0.2737i
0.96 0.28000 −2.655+0.3223i −2.654+0.3185i
0.92 0.39192 −2.689+0.3913i −2.686+0.3762i
0.87 0.49305 −2.731+0.4851i −2.724+0.4448i
0.75 0.66143 −2.835+0.7457i −2.807+0.5937i

(e). Numerical validation

To verify the theoretical results obtained in §3c, we adopt the following approach. We will compute numerical solutions of the system

U=0 3.40

and

Uτ+2z^×U+P=E2U+f(r)cos(ζτ), 3.41

i.e. the equations of motion for incompressible, rotating, viscous, small-amplitude motion. Our numerical method is based on a finite-volume algorithm for an unstructured set of control volumes [44]. We now prescribe the forcing f(r) to be of the following form:

f(r)=C(uk(r)+uk(r)), 3.42

where uk and uk are a pair of conjugate velocity eigenmodes of V~1, i.e. they are quadratic polynomials. We denote their corresponding eigenvalues as ±iλk. Furthermore, C is a constant whose exact value is not of major importance. As has been recently argued in the case of libration [45], the harmonic forcing f(r)cos(ζτ) can resonantly drive an inertial mode ul, provided the following two conditions are met:

  • (i) The integral Vulf(r)dV does not vanish. From (3.42) and the orthogonality property of inertial modes (2.8), it follows that f(r) can only enter in resonance with uk and uk.

  • (ii) The eigenfrequency λl and the driving frequency ζ should be (nearly) equal.

The above two conditions imply that resonance can only occur if ζ=±λk. We now verify whether this behaviour is recovered in the numerical solution for the choice of parameters c¯=1,β=0.45,E=5×104. For this parameter set, we find that one of the eigenmodes associated with the subspace V~1 is characterized by the eigenfrequency λk=±0.83236. This corresponds to figure 2c, and its meridional circulation pattern is similar to the one shown in figure 3c. Furthermore, the forcing f(r) corresponding to this eigenmode pair is

f(r)=C(0.82812yzx^0.48581xzy^+0.312166xyz^). 3.43

In figure 6, we show time series of the kinetic energy Ek=(1/2C2)V|U|2dV for different forcing frequencies ζ. We indeed find that resonance only takes place for ζk. Furthermore, in figure 7, we compare between numerically established profiles of Uz and theoretically obtained solutions for uz,k in the planes x=0 and y=0. We observe an excellent agreement between both profiles, except near the boundaries, where the numerical solution exhibits viscous Ekman layers. Our numerical findings are thus consistent with our theoretical arguments, i.e. the prescribed force f(r) can resonantly drive the mode uk, provided ζ=±λk. As such, our numerical calculations validate the theoretical results obtained in §3c.

Figure 6.

Figure 6.

Time series of the kinetic energy Ek for different forcing frequencies ζ and a spatial force density given by (3.43). (Online version in colour.)

Figure 7.

Figure 7.

Isocontours of the numerically established flow Uz (top half) at instant τ=92, and the theoretically computed z-component uz,k of the inertial mode uk (bottom half) in the planes x=0 (a) and y=0 (b). Both quantities have been normalized such that their value at the origin is 1. (Online version in colour.)

4. Completeness of the inertial modes

One of the major outstanding questions regarding the theory of inertial modes is whether they are complete. By the term complete, we mean that any sufficiently smooth solenoidal velocity field that satisfies the non-penetration condition can be expanded as a sum of inertial modes. This question was first raised by Greenspan in his now-classical monograph on rotating flows [32]. It has essentially remained unanswered until date, apart from a recent work that proved the completeness of inertial modes in a rotating annular duct [46]. The issue of completeness is not without interest, because such a property could provide a new paradigm for the solution of many fluid dynamic problems in rapidly rotating systems. Indeed, since the Coriolis force does not couple different inertial modes, an expansion in terms of inertial modes could provide a more efficient way to solve and understand the behaviour of rapidly rotating flows.

The approach presented in §3 and appendix A now allows us to shed some new light on this outstanding question. As a starting point, we recall that the eigenvalue problem yields a complete basis of eigenvectors for the subspace V~n. Since V~n is isomorf with W~n, it follows that the vorticity eigenmodes are a basis for W~n. This means that every solenoidal vector field w that is polynomial and of maximum degree n, can be expanded as a sum of inertial modes of W~n. In terms of the Mie representation, the toroidal and poloidal scalars of the vorticity eigenmodes of W~n span all scalar functions that are of the form ft, respectively, fs

ft(r,θ,ϕ)=k=0l+2knl=1nm=lltklmrl+2kYlm(θ,ϕ) 4.1

and

fs(r,θ,ϕ)=k=0l+2kn+1l=1n+1m=llsklmrl+2kYlm(θ,ϕ). 4.2

Taking the limit of n, we obtain the following expressions:

ft(r,θ,ϕ)=k=0l=1m=lltklmrl+2kYlm(θ,ϕ) 4.3

and

fs(r,θ,ϕ)=k=0l=1m=llsklmrl+2kYlm(θ,ϕ). 4.4

On the other hand, every function f that is square-integrable over the ellipsoidal volume under consideration, can be expanded as follows [43]:

f(r,θ,ϕ)=k=0l=0m=llfklmrl+2kYlm(θ,ϕ). 4.5

Comparing the above expression to (4.3) or (4.4), one finds that they only are different in the lower bound for the index l. Thus, given a square-integrable function f, one can define f

f(r,θ,ϕ)=f(r,θ,ϕ)k=0fk00r2k. 4.6

As such, f is of the form (4.3) or (4.4), and has thus a decomposition in terms of vorticity eigenmode toroidal or poloidal scalars. Furthermore, we note that

×fr=×fr. 4.7

This suggests that every vorticity field, for which both the toroidal and poloidal scalars are square-integrable functions, can be expanded in terms of vorticity eigenmodes. Given that the subspaces V~n and W~n are isomorf, this furthermore suggests that any, sufficiently smooth solenoidal velocity field that satisfies (2.6) can be expanded on a basis of inertial modes. However, a more rigorous proof is required to show exactly how the regularity and integrability constraints on the Mie scalars carry over to the vorticity field and its corresponding velocity field. Such a proof, however, is outside the scope of this work.

5. Integral properties

For inertial modes in rotating spheres and spheroids, it was shown [26,27] that the following identity holds for any inertial mode ul:

ul,2ul=ul2uldV=0. 5.1

We now argue that this integral also vanishes in rotating triaxial ellipsoids. Our line of thought is as follows. Since V~n2 is a subspace of V~n, V~n has an orthonormal basis of inertial modes {u1,u2,…,uk,uk+1,…,uN} such that {u1,u2,…,uk} is a basis for V~n2. We recall that, by virtue of the skew-Hermitian nature of the eigenvalue problem of which these modes are the eigenvectors, these (finite-dimensional) bases are complete. We now consider a certain inertial mode ul within the subspace V~n such that ul does not belong V~n2, i.e. with k<lN. Thus, ωl belongs to the subspace W~n, but not to W~n2. This is equivalent to saying that the cartesian components of its associated vorticity field ωl=∇×ul are polynomials of (exactly) degree n or n−1. Now, ∇2ul does not necessarily belong to V~n2. Indeed, nothing guarantees that ∇2ul satisfies the non-penetration condition (2.6). On the other hand, ∇2ωl=∇×∇2ul belongs to the subspace W~n2, as it is solenoidal and its polymomial degree is not higher than n−2. Now, we define

Ql1×2ωl. 5.2

By definition, the operator ∇−1× transforms elements of W~n2 into elements of V~n2. As such Ql belongs to V~n2, and thus satisfies the boundary condition (2.6), in contrast to ∇2ul. However, Ql and ∇2ul are connected by the following identity:

×Ql=×2ul=2ωl 5.3

and thus:

2ul=Qlψ. 5.4

As such, one can write

ul,2ul=ul,Qlul,ψ=ul,Ql. 5.5

Here, we have used the fact that

ul,ψ=ulψdV=0. 5.6

This integral vanishes because ul is solenoidal and satisfies the non-penetration condition (2.6). Now, since QlV~n2, we may write it as a sum of inertial modes ui of V~n2, i.e.

Ql=i=1kαiui. 5.7

This expansion finds it justification in the fact that the inertial modes ui of V~n2 are a complete basis for this vector space, as argued at the beginning of this section. This implies that (5.5) may be recast as

ul2uldV=i=1kαiuluidV. 5.8

Hence, since ul is orthogonal to every ui (1≤ik), every term in sum on the right-hand side of the above expression vanishes, and we recover (5.1). We find thus that this remarkable integral property also holds for rotating triaxial ellipsoids.

Furthermore, we find that integral (5.8) also vanishes if we replace ul by um, provided that um is an inertial mode that does not belong to V~n2. we can reformulate this as follows. The integral property

um2uldV=0 5.9

is satisfied if the highest polynomial order of the cartesian components of um is higher than n−2. This can be identified with another integral property postulated by Liao & Zhang [33]. In their notation, this is written as

umlM,2umlK=0,MK, 5.10

where the highest polynomial degree of umlK and umlM is 2K+m, respectively, 2M+m. Thus, the above arguments do extend the integral property discovered by Liao & Zhang [33] to triaxial ellipsoids.

6. Concluding remarks

In this work, we have outlined a procedure to compute inviscid inertial modes in a rotating triaxial ellipsoid. Analytic, explicit expressions for the eigenvalues can be obtained for a limited number of eigenmodes. We have illustrated this for velocity eigenmodes that are linear and quadratic in the cartesian coordinates. Furthermore, it is straightforward to extend our work to polynomial bases of higher degree. Indeed, using a clever combination of state-of-the art numerical and symbolical mathematical software, it is in principle possible to fully automate the procedure described in §3. Taking into account that the dimension of the subspaces increases rapidly with polynomial degree, and that the computational power to solve an eigenvalue problem scales as the third power of its dimension, this may rapidly become very involved. Nevertheless, computational power is so abundant these days that solving the eigenvalue problem up to degree 50 or so should not pose a major problem.

Furthermore, we have shown that two integral properties, originally postulated for inertial modes in spherical and spheroidal domains, also apply to triaxial ellipsoids. These properties reflect that the inertial modes are of polynomial nature. This, at its turn, is closely related to the fact that the solution of the Laplace equation for the gauge function (A 20) are ellipsoidal solid harmonics, which have a polynomial representation. In response to the question raised by Liao & Zhang [33], this is really the distinctive feature which makes these properties hold for ellipsoidal domains, and not e.g. for cylindrical ones. Finally, we have also addressed the question of completeness of inertial modes. Hopefully, our new insight is an impetus for a mathematically rigorous proof of a completeness theorem.

Possible applications of this work include the linear stability analysis of rotating flows in triaxial ellipsoids in terms of inertial modes. As mentioned in the Introduction, previous studies have been restricted to the limit of small deformation; using the present results, this can be extended to ellipsoids of arbitrary deformation. This in fact comes down to a reinterpretation of the works of Gledzer & Ponomarev [38], Wu & Roberts [40] and Roberts & Wu [47]. We are already undertaking such an effort for the case of flows driven by libration. Finally, a number of issues have remained unaddressed in this work. Although we have computed the leading order viscous correction to the eigenfrequency, one major task to be achieved is the calculation of the viscous Ekman boundary layer. In our understanding, this will necessitate the use of an ellipsoidal coordinate system, and appears a challenging problem.

Supplementary Material

Viscous correction of the spin-over mode
rspa20140093supp1.m (2.1KB, m)

Acknowledgements

I am indebted to David Cébron for enlightening and stimulating discussions, and to Elisabeth Canet, Andy Jackson and Jérôme Noir for feedback on first versions of this manuscript. I am grateful to three anonymous reviewers whose comments substantially helped to improve this article.

Appendix A. Vector spaces of polynomial solenoidal vector fields

In this section, we discuss the properties of the vector spaces Wn and Vn that are presented in §3a in more detail:

  • (i) We show that the elements wWn have a toroidal–poloidal representation (3.3) in which t and s are, respectively, homogeneous polynomials of degree n and n+1. To this end, we start from the well-known identities:
    2s=rw A 1
    and
    2t=r×w, A 2
    in which 2 denotes the ‘angular momentum operator’
    2=1r2sinθθ(sinθθ)1r2sin2θ2ϕ2. A 3
    Since wWn, the right-hand side of (A 1) and (A 2) are homogeneous polynomials of degree n+1 and n, respectively. Using the fact that the spherical harmonics have a polynomial representation [43], we may recast (A 1) and (A 2) as follows:
    2s=rn+1l=1mod(l,n)=1n+1m=llalmYlm(θ,ϕ) A 4
    and
    2t=rnl=1mod(l,n)=0nm=llblmYlm(θ,ϕ). A 5
    The absence of the l=0 harmonic in these expressions is due to the fact that w and ∇×w are solenoidal. Given that the spherical harmonics are eigenfunctions of the angular momentum operator, we immediately find
    s=rn+1l=1mod(l,n)=1n+1m=llalml(l+1)Ylm(θ,ϕ) A 6
    and
    t=rnl=1mod(l,n)=0nm=llblml(l+1)Ylm(θ,ϕ). A 7
    This is indeed of the form (3.4) and (3.5) with coefficients slm=alm/(l2+l) and tlm=blm/(l2+l).
  • (ii) The vector spaces Vn and Wn are isomorf. To prove this, we start from a toroidal–poloidal decomposition of vVn
    v=×T(r)r+××S(r)r. A 8
    Substituting this into w=∇×v, with w of the form (3.3), leads to
    T=s A 9
    and
    2S=t. A 10
    The Poisson equation (A 10) should be supplemented with a boundary condition such that v satisfies the boundary equation (2.6). Its general solution is of the form S=SP+SH, where SP is a particular solution of (A 10) and SH a harmonic function that allows to satisfy the boundary condition. With t of the form (3.4), a solution for SP is readily found
    SP=rn+2l=1mod(l,n)=0ntlm(n+3)(n+2)l(l+1)Ylm(θ,ϕ). A 11
    We now consider the following solenoidal vector field:
    v0=×T(r)r+××SP(r)r. A 12
    It follows that w=∇×v0. By virtue of the Helmholtz theorem, we know that any other vector field v that obeys w=∇×v is of the form
    v=v0ξ. A 13
    To fix the gauge function ξ, we require that v is solenoidal and satisfies (2.6). This leads to a Laplace equation for ξ
    2ξ=0, A 14
    with boundary condition
    n^ϕ=n^v0. A 15
    Since the right-hand side of (A 15) satisfies
    n^v0dS=v0dV=0, A 16
    problem (A 14) and (A 15) has a solution that is unique, up to an irrelevant additive constant. Thus for any element w of Wn, the corresponding element of Vn is uniquely determined, and this shows that both vector spaces are indeed connected by an isomorphism.
  • (iii) We now also argue that the elements v of Vn are polynomials of degree n+1. Using (3.5), (A 9) and (A 11), we find that the components of vector field v0 defined by (A 12) are homogeneous polynomials of degree n+1. The polynomial character of v now hinges on the nature of the solution for ξ of the problem (A 14) and (A 15). To this end, we introduce ellipsoidal coordinates (μ1,μ2,μ3) that are defined as follows [48]:
    x2a2+μ1+y2b2+μ1+z2c2+μ1=1, A 17
    x2a2+μ2+y2b2+μ2+z2c2+μ2=1 A 18
    andx2a2+μ3+y2b2+μ3+z2c2+μ3=1. A 19
    We can assume without loss of generality, a>b>c. Then, the following bounds apply: μ1>−c2, −c2>μ2>−b2, −b2>μ3>−a2. The surfaces of constant μ1 are confocal ellipsoids; in particular, the surface μ1=0 is the ellipsoidal surface defined by (2.1) The general solution of (A 14) within the interior of the ellipsoid is of the form [48]:
    ξ(μ1,μ2,μ3)=l=0m=12l+1AlmElm(μ1)Elm(μ2)Elm(μ3), A 20
    where the functions Elm denote Lamé functions of the first kind. It is furthermore well established that products of the form Elm(μ1)Elm(μ2)Elm(μ3) are polynomials of degree l in the cartesian coordinates; such products bear the name solid ellipsoidal harmonics. The boundary condition (A 15) now allows to determine the coefficients Alm. We can recast (A 15) as follows:
    ξμ1|μ1=0=(xa2x^+yb2y^+zc2z^)v0. A 21
    Using (A 20), the left-hand side can be further expanded as
    l=0m=12l+1AlmdElmdμ1|μ1=0Elm(μ2)Elm(μ3)=(xa2x^+yb2y^+zc2z^)v0. A 22
    Now, the right-hand side of this expression is a polynomial of degree n+2. According to Ferrers [49], this implies that the coefficients Alm are non-zero only if ln+2. Since the corresponding solid harmonic functions in (A 20) are polynomials of degree l, it follows that the solution for ξ is polynomial of (maximum) degree n+2. Hence, the components of v are of degree n+1.

Appendix B. Solution of the eigenvalue problem in V~0 and V~1

In this appendix, we provide more details about the computation of the eigenvalues and eigenmodes of the space V~0 and V~1. The first step required to fulfil this task consists of generating the basis vectors for the respective subspaces. In principle, one could follow the approach sketched in appendix A. However, a more convenient algorithm has been presented by Wu & Roberts [40]. They first compute the basis vectors V for the unit sphere (with respect to coordinates R=(X,Y,Z)), and then use the so-called Poincaré transformation [50]

V=(VX,VY,VZ)v=(vx,vy,vz)=(aVx,bVy,cVz) B 1

and

R=(X,Y,Z)r=(x,y,z)=(aX,bY,cZ), B 2

to transform V(R) into v(r), where the latter vector field is (i) solenoidal and (ii) satisfies the boundary condition (2.6) at the surface of the ellipsoid defined by (2.1) (with respect to the coordinates (x,y,z)). Furthermore, unlike the approach sketched in §3b, we will not make use of a set of orthogonal basis vectors. This would present a complication that is unnecessary, as eigenvalues and eigenmodes are invariant under a change of basis.

For the subspace V~0=V0, one has the basis vectors

v1=(0,zc2,yb2),v2=(zc2,0,xa2)andv3=(yb2,xa2,0). B 3

Any velocity field u in this subspace can thus be written as u=j=13γjvj. Substituting this form in the ‘vorticity’ form of the inertial mode equation (2.7), we obtain three scalar equations (one for each component of the vorticity) for the unknown coefficients γj. This can be written under the form

iλγk=j=13Mkjγj, B 4

with

M=(02b2b2+c202a2a2+c200000). B 5

The eigenvalues and eigenvectors of this system are then given by (3.21) and (3.25).

The subspace V~1 is the direct sum of V0 and V1 and is 11-dimensional. A set of basis vectors for V~1 is found by extending the basis (B 3) with the following vectors:

v4=(0,xzc2,xyb2),v5=(yzc2,0,xya2),v6=(zx,zy,c2(12x2a22y2b2z2c2)),v7=(zx,zy,c2(x2a2y2b2)),v8=(yx,b2(z2c2x2a2),yz),v9=(yx,b2(12x2a2y2b22z2c2),yz)andv10=(a2(1x2a22y2b22z2c2),xy,xz),v11=(a2(y2b2z2c2),xy,xz).} B 6

We substitute again u=j=111γjvj into (2.7). This gives rise to three scalar equations, one for each vorticity component ωk

iλj=111(Nkxjx+Nkyjy+Nkzjz+Nk0j)γj=j=111(Mkxjx+Mkyiy+Mkzjz+Mk0j)γj, B 7

This has to hold for any position (x,y,z) in space, and therefore splits into 12 equations of the form:

iλj=111Nkljγj=j=111Mkljγj, B 8

where l can each take the values x, y, z or 0. We recall that the basis vectors v1,2,3 are purely linear in the coordinates. Therefore, the coefficients Nklj and Mklj with j=1,2,3 are non-zero only if l=0. Conversely, the other basis vectors do not possess a linear term, and thus Nk0j and Mk0j are zero for j=4,…,11. This means that the linear system defined by (B 7) block-separates into two blocks, one corresponding to j=1,2,3, the other one to j=4,…,11. The first one is identical to (B 4) and (B 5); the second one consists of the nine equations

iλj=411Nkljγj=j=411Mkljγj, B 9

where l now only takes the values x, y and z. Among these equations, there is one hidden linear dependency. Indeed, since both the left- and right-hand sides of (2.7) are solenoidal by construction, one has the following identities for any j=1,2,…,8:

Mxxj+Myyj+Mzzj=0 B 10

and

Nxxj+Nyyj+Nzzj=0. B 11

In other words, the sum of the three equations for which k=l gives rise to the identity 0=0. One of these equations is thus a linear combination of the other ones, and should thus be left out. If one omits the equation for which k=l=z in (B 9), The resulting eigenvalue problem can be written as

iλj=411NKjγj=j=411MKjγj, B 12

with

N=(11B1A0000001B11A0000000014B12B00000014A12A0000000012BA1+4BA00000012BA14BA0000000014AB12AB0000001+4AB12AB) B 13

and

M=(0022000000220000020000002000000000000084000000220000480000002200). B 14

The characteristic polynomial of the matrix N−1M is given by (3.27). It is even and of degree eight. Hence, it is still possible to find explicit solutions for the eigenvalues, i.e. for the roots of this polynomial.

Funding statement

This work was partly funded by ERC grant 247303 ‘MFECE’.

References

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Supplementary Materials

Viscous correction of the spin-over mode
rspa20140093supp1.m (2.1KB, m)

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