ThreeDimensionalConfigurations/Challenges

From jetwiki
Jump to navigation Jump to search

Challenges Constructing Ellipsoidal-Like Configurations

First, let's review the three different approaches that we have described for constructing Riemann S-type ellipsoids. Then let's see how these relate to the technique that has been used to construct infinitesimally thin, nonaxisymmetric disks.

Riemann S-type Ellipsoids

Usually, the density, ρ, and the pair of axis ratios, b/a and c/a, are specified. Then, the Poisson equation is solved to obtain Φgrav in terms of A1, A2, and A3. The aim, then, is to determine the value of the central enthalpy, H0 — alternatively, the thermal energy density, Π — and the two parameters, Ωf and λ, that determine the magnitude of the velocity flow-field. Keep in mind that, as viewed from a frame of reference that is spinning with the ellipsoid (at angular frequency, Ωf), the adopted (rotating-frame) velocity field is,

𝐮

=

λ[ı^(ab)yȷ^(ba)x].

Hence, the inertial-frame velocity is given by the expression,

𝐯

=

𝐮+e^φΩfϖ.

While we will fundamentally rely on the (Ωf,λ) parameter pair to define the velocity flow-field, in discussions of Riemann S-type ellipsoids it is customary to also refer to the following two additional parameters: The (rotating-frame) vorticity,

ζ×𝐮

=

ı^[uzyuyz]+ȷ^[uxzuzx]+k^[uyxuxy]

 

=

k^[λ(ba+ab)];

and the dimensionless frequency ratio,

f

ζΩf.

2nd-Order TVE Expressions

As we have discussed in detail in an accompanying chapter, the three diagonal elements of the (3×3) 2nd-order tensor virial equation are sufficient to determine the equilibrium values of Π, Ω3, and ζ3.

Indices 2nd-Order TVE Expressions that are Relevant to Riemann S-Type Ellipsoids
i j
1 1

0

=

[3522πabcρ]Π+{Ω32+2[b2b2+a2]Ω3ζ3(2πGρ)A1}a2+[a2a2+b2]2ζ32b2

2 2

0

=

[3522πabcρ]Π+[b2b2+a2]2ζ32a2+{Ω32+2[a2a2+b2]Ω3ζ3(2πGρ)A2}b2

3 3

0

=

[3522πabcρ]Π(2πGρ)A3c2


The (i,j)=(3,3) element gives Π directly in terms of known parameters. The (1,1) and (2,2) elements can then be combined in a couple of different ways to obtain a coupled set of expressions that define Ω3 and fζ3/Ω3.


[b2a2b2+a2]fΩ32

=

πGρ[(A1A2)a2b2b2a2A3c2];

[ EFE, Chapter 7, §48, Eq. (34) ]

and,

Ω32{1+[a2b2(a2+b2)2]f2}

=

2πGρ(a2b2)[A1a2A2b2].

[ EFE, Chapter 7, §48, Eq. (33) ]


Ou's (2006) Detailed Force Balance

In a separate accompanying chapter, we have described in detail how Ou(2006) used, essentially, the HSCF technique to solve the detailed force-balance equations. Beginning with the,

Eulerian Representation
of the Euler Equation
as viewed from a Rotating Reference Frame

[vt]rot+(vrot)vrot=1ρPΦgravΩf×(Ωf×x)2Ωf×vrot,


it can be shown that, for the velocity fields associated with all Riemann S-type ellipsoids,

(vrot)vrot

=

[12λ2(x2+y2)];

Ωf×(Ωf×x)

=

+[12Ωf2(x2+y2)];

2Ωf×vrot

=

[Ωfλ(bax2+aby2)].

Hence, within each steady-state configuration the following Bernoulli's function must be uniform in space:

H+Φgrav12Ωf2(x2+y2)12λ2(x2+y2)+Ωfλ(bax2+aby2)

=

CB,

Ou(2006), p. 550, §2, Eq. (6)

where CB is a constant. So, at the surface of the ellipsoid (where the enthalpy H = 0) on each of its three principal axes, the equilibrium conditions demanded by the expression for detailed force balance become, respectively:

  1. On the x-axis, where (x, y, z) = (a, 0, 0):

    2[CBa2+(πGρ)IBT]

    =

    (2πGρ)A1Ωf2λ2+2Ωfλ(ba)

  2. On the y-axis, where (x, y, z) = (0, b, 0):

    2[CBa2+(πGρ)IBT]

    =

    (2πGρ)A2(b2a2)Ωf2(b2a2)λ2(b2a2)+2Ωfλ(ba)

  3. On the z-axis, where (x, y, z) = (0, 0, c):

    2[CBa2+(πGρ)IBT]

    =

    (2πGρ)A3(c2a2)

This third expression can be used to replace the left-hand-side of the first and second expressions. Then via some additional algebraic manipulation, the first and second expressions can be combined to provide the desired solutions for the parameter pair, (Ωf,λ), namely,

Ωf2(πGρ)

=

12[M+M24N2],

      and      

λ2(πGρ)

=

12[MM24N2],

Ou(2006), p. 551, §2, Eqs. (15) & (16)

where,

M

2[A1A2(b2a2)][a2a2b2],     and,

N

1ab(a2b2)[A3(a2b2)c2(A2A1)a2b2].

Hybrid Scheme

In a separate chapter we have detailed the hybrid scheme. For steady-state configurations, the three components of the combined Euler + Continuity equations give,

Hybrid Scheme Summary for Steady-State Configurations
k^:

(ρvz𝐮)

=

k^(ρ𝐚);

e^ϖ:

(ρvϖ𝐮)

=

e^ϖ(ρ𝐚)+vφ2ϖ;

e^φ:

(ρϖvφ𝐮)

=

e^φ(ρϖ𝐚).

In this context, the vector acceleration that drives the fluid flow is, simply,

𝐚

=

(H+Φgrav).

Then, for the velocity flow-patterns in Riemann S-type ellipsoids, we have,

(ρvz𝐮)

=

0           (because vz=0);

(ρvϖ𝐮)

=

λ2ϖ3[abba]{y4(ab)x4(ba)}ρ;

(ρϖvφ𝐮)

=

2λxyΩf[abba]ρ;

ϖvφ

=

[λ(ba)Ωf]x2[λ(ab)Ωf]y2.

Vertical Component:   Given that k^(ρ𝐚)=0, we deduce that,

H0

=

πGρc2A3.

Azimuthal Component:   Irrespective of the (x,y,z) location of each fluid element, this component requires,

abλΩf

=

πGρ[(A1A2)a2b2b2a2c2A3].

Radial Component:   After inserting the "azimuthal component" relation and marching through a fair amount of algebraic manipulation, we find that Irrespective of the (x,y,z) location of each fluid element, this component requires,

2πGρ(a2b2)[A1a2A2b2]

=

[λ2+Ωf2].

Compressible Structures

Here we draw heavily on the published work of Korycansky & Papaloizou (1996, ApJS, 105, 181; hereafter KP96) that we have reviewed in a separate chapter, and on the doctoral dissertation of Saied W. Andalib (1998).

Part I

Returning to the above-mentioned,

Eulerian Representation
of the Euler Equation
as viewed from a Rotating Reference Frame

𝐮t+(𝐮)𝐮=1ρPΦgravΩf×(Ωf×x)2Ωf×𝐮,

we next note — as we have done in our broader discussion of the Euler equation — that,

(𝐮)𝐮=12(𝐮𝐮)𝐮×(×𝐮)=12(u2)+ζ×𝐮,

where, as above, ζ×𝐮 is the vorticity. Making this substitution, we obtain what is essentially equation (7) of KP96, that is, the,

Euler Equation
written in terms of the Vorticity and
as viewed from a Rotating Reference Frame

𝐮t+(ζ+2Ωf)×𝐮=1ρP[Φ+12u212|Ωf×x|2] .

Hence, in steady-state, the Euler equation becomes,

FB+A=0,

where, the scalar "Bernoulli" function,

FB12u2+H+Φ12|Ωk^×x|2;

and,

A(ζ+2Ωf)×𝐮.


For later use …

  1. Curl of steady-state Euler equation:

    0

    =

    FB+𝐀

    0

    =

    ×[FB+𝐀]

    0

    =

    ×𝐀.

    This last step is justified because the curl of any gradient is zero.

  2. KP96 only deal with two-dimensional motion in the equatorial plane and, hence, there is no vertical motion:
    Hence, 𝐮 lies in the equatorial plane; both ζ and Ωf only have z-components; and, 𝐀 is perpendicular to both Ωf and 𝐮. Also, given that 𝐀 necessarily lies in the equatorial plane, its curl will only have a z-component, that is,

    ×𝐀=0

               

    [×𝐀]z=0.

  3. "Dot" 𝐮 into the steady-state Euler equation:

    0

    =

    FB+𝐀

    0

    =

    𝐮[FB+𝐀]

    0

    =

    𝐮FB.

    This last step is justified because 𝐀 is necessarily always perpendicular to 𝐮.




We will leave discussion of the Euler equation, for the moment, and instead look at the continuity equation. As viewed from the rotating frame of reference,

(ρ𝐮)t+(ρ𝐮)

=

0.

If we are able to write the momentum density (in the rotating frame) in terms of a stream-function, Ψ, such that,

ρ𝐮

=

×(k^Ψ)=ı^[Ψy]ȷ^[Ψx],

then satisfying the steady-state continuity equation is guaranteed because the divergence of a curl is always zero. Note, as well, that when written in terms of this stream-function, the z-component of the vorticity will be,

ζz

=

uyxuxy

 

=

x[1ρΨx]y[1ρΨy].

Note that the steady-state continuity equation may be rewritten in the form,

𝐮

=

𝐮[lnρ].




It can also be shown that the condition, [×𝐀]z=0 can be rewritten as,

𝐮

=

𝐮[ln(2Ωf+ζz].

By combining these last two expressions, we appreciate that,

𝐮ln[(2Ωf+ζz)ρ]

=

0.

This means that, in the steady-state flow whose spatial structure we are seeking, the velocity vector, 𝐮 (and also the momentum density vector, ρ𝐮) must everywhere be tangent to contours of constant vortensity, [(2Ωf+ζz)/ρ].

We need a function g(Ψ) such that,

g(Ψ)

=

1ρ{ζz+2Ωf}

 

=

1ρ{2Ωfx[1ρΨx]y[1ρΨy]}.

Let's try, Ψ=ρ2, and

ρ

=

ρc{1[y2b2+x2a2]}

2ρx2=x{2ρcxa2}=2ρca2

    and,    

2ρy2=y{2ρcyb2}=2ρcb2.

Then,

g(Ψ)

=

1ρ{2Ωfx[1ρρ2x]y[1ρρ2y]}

 

=

1ρ{2Ωf2[2ρx2]2[2ρy2]}

 

=

1ρ{2Ωf+4ρc[1a2+1b2]}.

Hence,

g(Ψ)

=

{2Ωf+4ρc[1a2+1b2]}Ψ1/2.

Next, given that,

dFBdΨ

=

g(Ψ),

we conclude that, to within an additive constant,

FB(Ψ)

=

g(Ψ)dΨ=g0Ψ1/2dΨ

 

=

2g0Ψ1/2

 

=

2g0ρ,

where,

g0

{2Ωf+4ρc[1a2+1b2]}.

Here's what to do:

Given g(Ψ), write out the functional forms of 𝐀 and FB(Ψ). Then see if FB=𝐀.

Part II

Consider a steady-state configuration that is the compressible analog of a Riemann S-type ellipsoid; even better, give the configuration a "peanut" shape rather than the shape of an ellipsoid. As viewed from a frame that is spinning with the configuration's overall angular velocity, Ωf=k^Ωf, generally we expect the configuration's internal (and surface) flow to be represented by a set of nested stream-lines and at every (x,y) location the fluid's velocity (and its momentum-density vector) will be tangent to the stream-line that runs through that point. It is customary to represent the stream-function by a scalar quantity, Ψ(x,y), appreciating that each stream-line will be defined by a curve, Ψ=constant; also, the local spatial gradient of Ψ(x,y) will be perpendicular to the local stream-line, hence it will be perpendicular to the local velocity vector as well. If we specifically introduce the stream-function via the relation,

ρ𝐮

=

×(k^Ψ)=ı^[Ψy]ȷ^[Ψx],

it will display all of the just-described attributes and we are also guaranteed that the steady-state continuity equation will be satisfied everywhere, because the divergence of a curl is always zero.

We also have demonstrated that the vector, 𝐀, has the right properties if,

𝐮ln[(2Ωf+ζz)ρ]

=

0.

This means that, at every location in the plane of the fluid flow, the gradient of the vortensity also must be perpendicular to the velocity vector. This constraint can be immediately satisfied if we simply demand that the vortensity be a function of the stream-function, Ψ, that is, we need,

(2Ωf+ζz)ρ

=

g(Ψ).

In other words, the scalar vortensity is constant along each stream-line. And, once we have determined the mathematical expression for this function, we will know that,

𝐀

=

[k^g(Ψ)]×ρ𝐮;

Furthermore, we should be able to determine the mathematical expression for FB(x,y) because,

dFBdΨ

=

g(Ψ).

As a check, we should find that,

FB+𝐀

=

0.

Part III

Here we closely follow Chapter 4 of Saied W. Andalib (1998).

From §4.1 (p. 80): "Euler's equation, the equation of continuity, the Poisson equation and the equation of state … govern the dynamics and evolution of these equilibrium configurations."

Equation of Continuity

In steady state, (ρ𝐮)/t=0. Hence the rotating-frame-based continuity equation becomes,

(ρ𝐮)

=

0.

If we insist that the momentum-density vector be expressible in terms of the curl of a vector — for example,

ρ𝐮

=

×𝔍,

Saied W. Andalib (1998), §4.1, p. 80, Eq. (4.1)

then satisfying this steady-state continuity equation is guaranteed because the divergence of a curl is always zero. "The task of satisfying the steady-state equation of continuity then shifts to identifying an appropriate expression for the vector potential, 𝔍." In the most general case, in terms of this vector potential the three Cartesian components of the momentum-density vector are,

ρux

=

𝔍zy𝔍yz;

ρuy

=

𝔍xz𝔍zx;

ρuz

=

𝔍yx𝔍xy.

Here, we will follow Andalib's lead and only look for fluid flows with no vertical motions. That is to say, we will set ρuz=0, in which case this last expression establishes the constraint,

𝔍yx

=

𝔍xy.

"A general solution to this equation can be found only if there exists a scalar function Γ(x,y,z) such that …"

𝔍y=Γy

      and,      

𝔍x=Γx;

note that this adopted functional behavior works because the constraint becomes,

2Γxy

=

2Γyx.

Hence, the expressions for the x- and y-components of the momentum-density vector may be rewritten, respectively, as,

ρux

=

𝔍zyz[Γy]=+y[𝔍zΓz];

ρuy

=

z[Γx]𝔍zx=x[𝔍zΓz].

If we again follow Andalib's lead and only look for models in which the x-y-plane flow is independent of the vertical coordinate, z, then, 𝔍z and Γ/z must be functions of x and y only. Therefore, 𝔍z is independent of z and Γ is at most linear in z. Now, rather than focusing on the determination of Γ(x,y), we can just as well define the scalar function,

Ψ(x,y)

𝔍zΓz,

in which case "… the components of the momentum density may be written as:"

ρ𝐮

=

ı^Ψyȷ^Ψx.

It is straightforward to demonstrate that this expression for the momentum-density vector does satisfy the steady-state continuity equation. "The function Ψ(x,y) will serve a similar role as the velocity potential for incompressible fluids."

Related Useful Expressions

Given that, by our design, the fluid motion will be confined to the x-y-plane, the fluid vorticity will have only a z-component; that is,

ζ=×𝐮=k^ζz,

where,

ζz

=

uyxuxy.

And when it is written in terms of Ψ(x,y), this z-component of the vorticity will be obtained from the expression,

ζz

=

x[1ρΨx]y[1ρΨy].

This is useful to know because, in the Euler equation (see immediately below) we will encounter a term that involves the cross product of the vector, (ζ+2Ω), with the rotating-frame-based velocity vector. Appreciating as well that the vector, Ω=k^Ωf, only has a nonzero z-component, we recognize that this term may be written as,

(ζ+2Ω)×𝐮

=

k^[(ζz+2Ωf)ρ]×[ı^Ψyȷ^Ψx]

 

=

[(ζz+2Ωf)ρ][ȷ^Ψy+ı^Ψx]

 

=

[(ζz+2Ωf)ρ]Ψ.

Saied W. Andalib (1998), §4.2, p. 83, Eq. (4.13)

Euler Equation

We begin with the,

Euler Equation
written in terms of the Vorticity and
as viewed from a Rotating Reference Frame

𝐮t+(ζ+2Ωf)×𝐮=1ρP[Φ+12u212|Ωf×x|2] .

Next, we rewrite this expression to incorporate the following three realizations:

  • For a barotropic fluid, the term involving the pressure gradient can be replaced with a term involving the enthalpy via the relation, H=P/ρ.
  • The expression for the centrifugal potential can be rewritten as, 12|Ωf×x|2=12Ωf2(x2+y2).
  • In steady state, 𝐮/t=0.

This means that,

(ζ+2Ωf)×𝐮

=

[H+Φgrav+12u212Ωf2(x2+y2)].

If the term on the left-hand-side of this equation can be expressed in terms of the gradient of a scalar function, then it can be readily grouped with all the other terms on the right-hand-side, which already are in the gradient form.

Striving for Gradient Form

As we have already demonstrated above, the term on the left-hand-side of the Euler equation can be rewritten as,

(ζ+2Ω)×𝐮

=

[(ζz+2Ωf)ρ]Ψ.

If the term inside the square brackets on the right-hand-side were a constant — that is, independent of position — then it could immediately be moved inside the gradient operator and we will have accomplished our objective. But, while Ωf is constant "… generally the vorticity and density are both functions of x and y." As Andalib has explained, "The expression … can be cast in the form of a gradient only if

[(ζz+2Ωf)ρ]

=

g(Ψ),

where g is an arbitrary function." Specifically in this case, the term on the left-hand-side of the Euler equation may be written as,

(ζ+2Ω)×𝐮

=

FB(Ψ)

 

=

[dFB(Ψ)dΨ]Ψ.

That is, we accomplish our objective by recognizing that the sought-after function, FB(Ψ), is obtained from g(Ψ) via the relation,

dFB(Ψ)dΨ

=

g(Ψ).


For example, try …

FB(Ψ)

=

C0Ψ+12C1Ψ2

Saied W. Andalib (1998), §4.3, p. 85, Eq. (4.22)

g(Ψ)

=

C0+C1Ψ.

This means that,

[(ζz+2Ωf)ρ]

=

C0+C1Ψ

2ΩfC0ρ

=

C1ρΨζz

 

=

C1ρΨ+x[1ρΨx]+y[1ρΨy].

Saied W. Andalib (1998), §4.3, p. 85, Eq. (4.24)


Having transformed the left-hand-side term into the gradient of the scalar function, FB(Ψ), the Euler equation can now be written as,

[H+Φgrav+FB(Ψ)+12u212Ωf2(x2+y2)]

=

0

H+Φgrav+FB(Ψ)+12u212Ωf2(x2+y2)

=

CB,

where we will refer to CB as the Bernoulli constant.

Strategy

STEP 0:  Choose the pair of model-sequence parameters, (C0,C1), that are associated with the function, FB(Ψ). Hold these fixed during iterations.

STEP 1:  Guess a density distribution, ρ(x,y). For example, pick the equatorial-plane (uniform) density distribution of a Riemann S-type ellipsoid with an equatorial-plane axis-ratio, b/a and meridional-plane axis-ratio, c/a; use the same b/a ratio to define two points on the configuration's surface throughout the iteration cycle.

STEP 2:  Given ρ(x,y), solve the Poisson equation to obtain, Φgrav(x,y). In the first iteration, this should exactly match the A1,A2,A3 values associated with the chosen Riemann S-type ellipsoid.

STEP 3:  Guess a value of Ωf — perhaps the spin-frequency associated with your "initial guess" Riemann ellipsoid — then solve the following two-dimensional, elliptic PDE to obtain Ψ(x,y)

2ΩfC0ρ

=

C1ρΨ+x[1ρΨx]+y[1ρΨy].

Boundary Condition

Moving along various rays from the center of the configuration, outward, the surface is determined by the location along each ray where H(x,y) goes to zero for the first time. We set Ψ=0 at these various surface locations. At each of these locations, the velocity vector must be tangent to the surface. This requirement also, then, sets the value of Ψ/y and Ψ/x at each location.

STEP 4:  Determine (rotating-frame) velocity from knowledge of Ψ(x,y) and ρ(x,y).

𝐮

=

1ρ{ı^[Ψy]ȷ^[Ψx]}

u2=𝐮𝐮

=

1ρ2{[Ψy]2+[Ψx]2}.

STEP 5:  Using the "scalar Euler equation,"

H+Φgrav+C0Ψ+12C1Ψ2+12u212Ωf2(x2+y2)

=

CB,

Saied W. Andalib (1998), §4.3, p. 85, Eq. (4.23)
  • Set H=0 at two different points on the surface of the configuration — usually at (x,y)=(a,0) and (x,y)=(0,b) — to determine values of the two constants, Ωf2 and CB.
  • At all points inside the configuration, determine H(x,y).

STEP 6:  Use the barotropic equation of state to determine the "new" mass-density distribution from the knowledge of the enthalpy, H(x,y).

Compare

Incompressible

𝐮

=

λ[ı^(ab)yȷ^(ba)x].

u2𝐮𝐮

=

λ2[b2(x2a2)+a2(y2b2)].

ζ×𝐮

=

ı^[uzyuyz]+ȷ^[uxzuzx]+k^[uyxuxy]

 

=

k^[λ(ba+ab)].

ζ×𝐮

=

λ2(ba+ab)[ı^(ba)x+ȷ^(ab)y]

 

=

{λ2(a2+b2)2[x2a2+y2b2]}.

Returning to the above-mentioned,

Eulerian Representation
of the Euler Equation
as viewed from a Rotating Reference Frame

𝐮t+(𝐮)𝐮=1ρPΦgravΩf×(Ωf×x)2Ωf×𝐮,

we next note — as we have done in our broader discussion of the Euler equation — that,

(𝐮)𝐮=12(𝐮𝐮)𝐮×(×𝐮)=12(u2)+ζ×𝐮.

Making this substitution, we obtain

𝐮t+[12(u2)+ζ×𝐮]

=

1ρPΦgravΩf×(Ωf×x)2Ωf×𝐮

it can be shown that, for the velocity fields associated with all Riemann S-type ellipsoids,

(vrot)vrot

=

[12λ2(x2+y2)];

Ωf×(Ωf×x)

=

+[12Ωf2(x2+y2)];

2Ωf×vrot

=

[Ωfλ(bax2+aby2)].

As a check,

(𝐮)𝐮

=

12(u2)+ζ×𝐮

=

{λ22[b2(x2a2)+a2(y2b2)]λ2(a2+b2)2[x2a2+y2b2]}

 

=

λ22{(x2+y2)}.

Yes! This expression matches the one that appears just a few lines earlier in this discussion.

Now, let's switch the order of terms in the steady-state Euler equation to permit an easier comparison with our attempt to develop the compressible models.

𝐮t+[12(u2)+ζ×𝐮]

=

1ρPΦgravΩf×(Ωf×x)2Ωf×𝐮

0

=

[H+Φgrav+12u212Ωf2(x2+y2)](ζ+2Ωf)×𝐮.

Compressible

Now in our above discussion of Andalib's work, the steady-state form of the Euler equation was formulated as,

[H+Φgrav+FB(Ψ)+12u212Ωf2(x2+y2)]

=

0.

It is easy to appreciate that,

FB(Ψ)

=

(ζ+2Ωf)×𝐮.

As we have shown, in the case of the incompressible (Riemann S-type ellipsoid) models,

(ζ+2Ωf)×𝐮

=

{λ2(a2+b2)2[x2a2+y2b2]+[Ωfλ(bax2+aby2)]}.

If we attempt to directly relate these two expressions, we must acknowledge that,

FB(Ψ)

=

λ2(a2+b2)2[x2a2+y2b2]+[Ωfλ(bax2+aby2)]

 

=

x2a2[12λ2(a2+b2)+Ωfλab]+y2b2[12λ2(a2+b2)+Ωfλab].

As we have discussed above, Andalib (1998) found that some interesting model sequences could be constructed if he adopted the functional form,

FB(Ψ)

=

C0Ψ+12C1Ψ2.

Evidently, the incompressible (uniform-density) Riemann S-type ellisoids can be retrieved from our derived compressible-model formalism if we set, C1=0, and,

Ψ(x,y)

=

x2a2+y2b2,

with,

C0

=

[12λ2(a2+b2)+Ωfλab]

=

ζz2(a2b2a2+b2)[2Ωfζz].

Afterthought:  Because we want Ψ(x,y) to go to zero at the surface, it likely will be better to set,

Ψ1[x2a2+y2b2],

then adjust the sign of C0 and add a constant (zeroth-order term) to the definition of FB(Ψ).

Trial #1

Restricting our discussion to nonaxisymmetric, thin disks, let's assume ρ is uniform throughout the configuration and that,

Ψ(x,y)

=

Ψ0[1(x2a2+y2b2)].

This means that,

Ψx=Ψ0(2xa2)

      and,      

Ψy=Ψ0(2yb2).

The momentum density vector is governed by the relation,

ρ𝐮

=

ı^[Ψy]ȷ^[Ψx]

 

=

Ψ0{ı^[2yb2]+ȷ^[2xa2]}.

[Ψ has units of "density × length2 per time"]

First of all, let's see if the steady-state continuity equation is satisfied:

(ρ𝐮)

=

(ρux)x+(ρuy)y

 

=

ρ{uxx+uyy}

 

=

Ψ0ρ{x[2yb2]+y[2xa2]}

 

=

0.      Q.E.D.

Next, let's determine the z-component of the vorticity and the vortensity:

ζz

=

uyxuxy

 

=

Ψ0{x[2xρa2]+y[2yρb2]}

 

=

2Ψ0ρ[1a2+1b2];

(ζz+2Ωf)ρ

=

1ρ{2Ψ0ρ[1a2+1b2]+2Ωf}.

This means that,

(ζ+2Ω)×𝐮

=

{(ζz+2Ωf)ρ}k^×(ρ𝐮)

 

=

Ψ0{(ζz+2Ωf)ρ}k^×{ı^[2yb2]+ȷ^[2xa2]}

 

=

2Ψ0[(ζz+2Ωf)ρ][ı^(xa2)+ȷ^(yb2)].

But this entire process was designed to ensure that,

(ζ+2Ω)×𝐮

=

FB(Ψ),

where, FB(Ψ)C0Ψ. Let's see if we get the same expression …

FB(Ψ)

=

[ı^x+ȷ^y]C0Ψ

 

=

C0Ψ0[ı^x+ȷ^y][1(x2a2+y2b2)]

 

=

2C0Ψ0[ı^(xa2)+ȷ^(yb2)].

This is indeed the same expression as above if we set,

C0

=

(ζz+2Ωf)ρ.

Hooray!!

Finally, let's make sure that the elliptic PDE "constraint" equation is satisfied.

2Ωf

=

C0ρ+C1ρΨ+x[1ρΨx]+y[1ρΨy]

 

=

(ζz+2Ωf)+C1ρΨx[Ψ0ρ2xa2]y[Ψ0ρ2yb2]

 

=

ζz+2Ωf[Ψ0ρ2a2][Ψ0ρ2b2]

 

=

ζz+2Ωf2Ψ0ρ[1a2+1b2]

 

=

2Ωf.       Yes!

Trial #2

Still restricting our discussion to nonaxisymmetric, thin disks, let's try, Ψ=Ψ0(ρ/ρc)2, and

ρ

=

ρc{1[y2b2+x2a2]}

2ρx2=x{2ρcxa2}=2ρca2

    and,    

2ρy2=y{2ρcyb2}=2ρcb2.

IMPORTANT NOTE (by Tohline on 22 September 2020):    As I have come to appreciate today — after studying the relevant sections of both EFE and BT87 — this is an example of a heterogeneous density distribution whose gravitational potential has an analytic prescription. As is discussed in a separate chapter, the potential that it generates is sometimes referred to as a Ferrers potential, for the exponent, n = 1.

In our accompanying discussion we find that,

Φgrav(𝐱)(πGρc)

=

12IBTa12(A1x2+A2y2+A3z2)+(A12x2y2+A13x2z2+A23y2z2)+16(3A11x4+3A22y4+3A33z4),

where,

for ij

Aij

AiAj(ai2aj2)

[ EFE, §21, Eq. (107) ]
for i=j

2Aii+=13Ai

=

2ai

[ EFE, §21, Eq. (109) ]

More specifically, in the three cases where the indices, i=j,

3A11

=

2a12(A12+A13),

3A22

=

2a22(A21+A23),

3A33

=

2a32(A31+A32).

This means that,

Ψx=(Ψ0ρc2)2ρρx=2ρ(2ρcxa2)(Ψ0ρc2)

      and,      

Ψy=(Ψ0ρc2)2ρρy=2ρ(2ρcyb2)(Ψ0ρc2).

 

The Elliptic PDE Constraint Equation

2Ωf

=

C0ρ+C1ρΨ+x[1ρΨx]+y[1ρΨy]

 

=

C0ρx[(4xa2)(Ψ0ρc)]y[(4yb2)(Ψ0ρc)]

 

=

C0ρ4Ψ0ρc[1a2+1b2]


The momentum density vector is governed by the relation,

ρ𝐮

=

ı^[Ψy]ȷ^[Ψx]

 

=

ı^[2ρ(2ρcyb2)(Ψ0ρc2)]+ȷ^[2ρ(2ρcxa2)(Ψ0ρc2)]

 

=

ρ{ı^[4Ψ0yρcb2]+ȷ^[4Ψ0xρca2]}.

[Ψ has units of "density × length2 per time"]

As above, let's see if the steady-state continuity equation is satisfied:

(ρ𝐮)

=

(ρux)x+(ρuy)y

 

=

x[4Ψ0yρρcb2]+y[4Ψ0xρρca2]

 

=

4Ψ0ρc{yb2ρx+xa2ρy}

 

=

4Ψ0ρc{yb2[2ρcxa2]xa2[2ρcyb2]}

 

=

0.      Yes!

Next, as above, let's determine the z-component of the vorticity and the vortensity:

ζz

=

uyxuxy

 

=

4Ψ0ρc{x[xa2]+y[yb2]}

 

=

4Ψ0ρc[1a2+1b2].

(ζz+2Ωf)ρ

=

1ρ{4Ψ0ρc[1a2+1b2]+2Ωf}.

This means that,

(ζ+2Ω)×𝐮

=

{(ζz+2Ωf)ρ}k^×(ρ𝐮)

 

=

4Ψ0(ζz+2Ωf)ρck^×{ı^[yb2]+ȷ^[xa2]}

 

=

4Ψ0(ζz+2Ωf)ρc{ı^[xa2]+ȷ^[yb2]}

Now, let's examine the gradient of FB(Ψ).

FB(Ψ)

=

[ı^x+ȷ^y]C0Ψ

 

=

C0Ψ0ρc2[ı^ρ2x+ȷ^ρ2y]

 

=

2C0ρΨ0ρc2{ı^[2ρcxa2]ȷ^[2ρcyb2]}

 

=

4C0ρΨ0ρc{ı^[xa2]+ȷ^[yb2]},

which is identical to the immediately preceding expression if we set,

C0

=

(ζz+2Ωf)ρ.

Continuing with the above examination of the elliptic PDE "constraint" equation, we find that,

2Ωf

=

C0ρζz

 

=

(2Ωf+ζz)ζz

 

=

2Ωf.      Hooray!

Trial #3

If the density distribution has been specified, then Ψ is the "stream-function" from which all rotating-frame velocities are determined. Specifically,

𝐮

=

1ρ[ı^Ψyȷ^Ψx].

Most importantly, as has been detailed above, the term on the left-hand-side of the steady-state Euler equation becomes,

(ζ+2Ω)×𝐮

=

[(ζz+2Ωf)ρ]Ψ,

Saied W. Andalib (1998), §4.2, p. 83, Eq. (4.13)

where,

ζz

=

x[1ρΨx]y[1ρΨy].

Still restricting our discussion to infinitesimally thin, nonaxisymmetric disks, let's assume that,

ρ

=

ρc[1(x2a2+y2b2)]

ρx=(2ρcxa2)

    and,    

ρy=(2ρcyb2);

2ρx2=x{2ρcxa2}=2ρca2

    and,    

2ρy2=y{2ρcyb2}=2ρcb2.

And, let's assume that,

Ψ

=

Ψ0(ρρc)q,

Ψx

=

ρq1(qΨ0ρcq)ρx=ρq1(qΨ0ρcq)(2ρcxa2)=(ρρc)q1(2qΨ0xa2);

and, similarly,       Ψy

=

(ρρc)q1(2qΨ0yb2).

This means that,

𝐮

=

1ρ{ı^[(ρρc)q1(2qΨ0yb2)]ȷ^[(ρρc)q1(2qΨ0xa2)]}

𝐮𝐮

=

1ρ2{[(ρρc)q1(2qΨ0yb2)]2+[(ρρc)q1(2qΨ0xa2)]2}.

It also means that,

ζz

=

x[(ρρc)q2(2qΨ0xρca2)]+y[(ρρc)q2(2qΨ0yρcb2)]

 

=

(ρρc)q2(2qΨ0ρca2)+(2qΨ0xρca2)x(ρρc)q2+(ρρc)q2(2qΨ0ρcb2)+(2qΨ0yρcb2)y(ρρc)q2

 

=

(ρρc)q2(2qΨ0ρc)[1a2+1b2]+(2qΨ0xρca2)[(q2)ρc2qρq3ρx]+(2qΨ0yρcb2)[(q2)ρc2qρq3ρy]

 

=

(ρρc)q2(2qΨ0ρc)[1a2+1b2](2qΨ0xρc2a2)[(q2)(ρρc)q32ρcxa2](2qΨ0yρc2b2)[(q2)(ρρc)q32ρcyb2]

 

=

qΨ0ρc{2(ρρc)q2[1a2+1b2](2xa2)[(q2)(ρρc)q32xa2](2yb2)[(q2)(ρρc)q32yb2]}

 

=

qΨ0ρc(ρρc)q3[2(ρρc)(1a2+1b2)4(q2)(x2a4)4(q2)(y2b4)]

Hence,

(ζ+2Ω)×𝐮

=

[ı^Ψx+ȷ^Ψy]{2Ωfρc(ρρc)1+(ρρc)1ζzρc}

 

=

[ı^(ρρc)q1(2qΨ0xa2)+ȷ^(ρρc)q1(2qΨ0yb2)]{2Ωfρc(ρρc)1

 

 

+qΨ0ρc2(ρρc)q4[2(ρρc)(1a2+1b2)4(q2)(x2a4)4(q2)(y2b4)]}

 

=

2qΨ0[ı^(xa2)+ȷ^(yb2)](ρρc)q2{2Ωfρc

 

 

+qΨ0ρc2(ρρc)q3[2(ρρc)(1a2+1b2)4(q2)(x2a4)4(q2)(y2b4)]}.

Exponent q = 2

Notice that, if q=2,

[(ζ+2Ω)×𝐮]q=2

=

8Ψ0ρc{Ωf+2Ψ0ρc(1a2+1b2)}[ı^(xa2)+ȷ^(yb2)].

Now, if we choose a function,

FB(Ψ)

=

D12Ψ1/2=D12Ψ01/2(ρρc)=D12Ψ01/2[1(x2a2+y2b2)],

we obtain,

FB(Ψ)

=

D12Ψ01/2(x2a2+y2b2)

 

=

D1Ψ01/2[ı^(xa2)+ȷ^(yb2)].

This is consistent with the elliptic PDE constraint if,

D1

=

8Ψ01/2ρc{Ωf+2Ψ0ρc(1a2+1b2)}.

Also if q=2, we have,

𝐮

=

1ρ{ı^Ψyȷ^Ψx}

 

=

1ρ{ı^(ρρc)(2qΨ0yb2)+ȷ^(ρρc)(2qΨ0xa2)}

 

=

{ı^(4Ψ0yρcb2)+ȷ^(4Ψ0xρca2)}

𝐮𝐮

=

(4Ψ0yρcb2)2+(4Ψ0xρca2)2

 

=

(4Ψ0ρc)2[x2a4+y2b4].

Keep in mind that, as discussed above, we are trying to satisfy the scalar Bernoulli relation,

CBHΦgrav

=

FB(Ψ)+12u212Ωf2(x2+y2)

 

=

4Ψ0ρc{Ωf+2Ψ0ρc(1a2+1b2)}[1(x2a2+y2b2)]+12(4Ψ0ρc)2[x2a4+y2b4]12Ωf2(x2+y2).

The right-hand-side of this expression does not appear to be rich enough to balance the gravitational potential (on the left-hand-side) which, as detailed above, contains x2y2 and x4 and y4 terms.


Exponent q = 3

Alternatively, if q=3,

[(ζ+2Ω)×𝐮]q=3

=

6Ψ0[ı^(xa2)+ȷ^(yb2)](ρρc){2Ωfρc+3Ψ0ρc2[2(ρρc)(1a2+1b2)4(x2a4)4(y2b4)]}

 

=

6Ψ0{2Ωfρc(ρρc)12Ψ0ρc2[x2a4+y2b4](ρρc)+6Ψ0ρc2(1a2+1b2)(ρρc)2}f^,

where,

f^

[ı^(xa2)+ȷ^(yb2)].

If we choose a function,

FB(Ψ)

=

D1Ψ2/3+D2Ψ

 

=

D1Ψ02/3(ρρc)2+D2Ψ0(ρρc)3,

we obtain,

FB(Ψ)

=

[2D1Ψ02/3(ρρc)+3D2Ψ0(ρρc)2](x2a2+y2b2)

 

=

{2D1Ψ02/3[1(x2a2+y2b2)]+3D2Ψ0[1(x2a2+y2b2)]2}[ı^(2xa2)+ȷ^(2yb2)]

 

=

{2D1Ψ02/3[1(x2a2+y2b2)]+3D2Ψ0[12(x2a2+y2b2)+(x2a2+y2b2)2]}[ı^(2xa2)+ȷ^(2yb2)]

 

=

{(2D1Ψ02/3+3D2Ψ0)(2D1Ψ02/3+6D2Ψ0)(x2a2+y2b2)+3D2Ψ0(x2a2+y2b2)2}f^

 

=

{(2D1Ψ02/3+3D2Ψ0)(2D1Ψ02/3+6D2Ψ0)(x2a2+y2b2)+3D2Ψ0[x4a4+2(x2y2a2b2)+y4b4]}f^.




Let's reorganize and expand the terms in both of these expressions in order to ascertain whether or not they can be matched. First …

[(ζ+2Ω)×𝐮]q=3

=

6Ψ0{2Ωfρc[1(x2a2+y2b2)]12Ψ0ρc2[x2a4+y2b4][1(x2a2+y2b2)]

 

 

+6Ψ0ρc2(1a2+1b2)[1(x2a2+y2b2)]2}f^,

 

=

6Ψ0{2Ωfρc2Ωfρc(x2a2+y2b2)12Ψ0ρc2[x2a4+y2b4]+12Ψ0ρc2[x2a4+y2b4](x2a2+y2b2)

 

 

+6Ψ0ρc2(1a2+1b2)[12(x2a2+y2b2)+(x2a2+y2b2)2]}f^,

 

=

6Ψ0{[2Ωfρc+6Ψ0ρc2(a2+b2)a2b2][2Ωfρc+12Ψ0ρc2(1a2+1b2)](x2a2+y2b2)

 

 

12Ψ0ρc2(x2a4+y2b4)+12Ψ0ρc2(x4a6+x2y2a4b2+x2y2a2b4+y4b6)+6Ψ0ρc2(1a2+1b2)(x4a4+2x2y2a2b2+y4b4)}f^,

In order for the zeroth-order terms to match, we need,

2D1Ψ02/3+3D2Ψ0

=

6Ψ0{2Ωfρc+6Ψ0ρc2(a2+b2)a2b2}

2D1Ψ02/3

=

3Ψ0{4Ωfρca2b2ρc2a2b2+12Ψ0(a2+b2)ρc2a2b2}3D2Ψ0

 

=

3Ψ0{4Ωfρca2b2ρc2a2b2+12Ψ0(a2+b2)ρc2a2b2D2}.

Then we also need,

6D2Ψ0

=

6Ψ0[2Ωfρc+12Ψ0ρc2(1a2+1b2)]2D1Ψ02/3

 

=

6Ψ0[2Ωfρc+12Ψ0ρc2(1a2+1b2)]3Ψ0{4Ωfρca2b2ρc2a2b2+12Ψ0(a2+b2)ρc2a2b2D2}

3D2Ψ0

=

6Ψ0[2Ωfρca2b2ρc2a2b2+12Ψ0ρc2(a2+b2)a2b2]6Ψ0[2Ωfρca2b2ρc2a2b2+6Ψ0(a2+b2)ρc2a2b2]

 

=

6Ψ0[6Ψ0(a2+b2)ρc2a2b2]

D2

=

12Ψ0(a2+b2)ρc2a2b2.

Finally, we need,

3D2Ψ0[x4a4+2(x2y2a2b2)+y4b4]16Ψ0

=

12Ψ0ρc2(x2a4+y2b4)+12Ψ0ρc2(x4a6+x2y2a4b2+x2y2a2b4+y4b6)+6Ψ0ρc2(1a2+1b2)(x4a4+2x2y2a2b2+y4b4)

(a2+b2)a2b2[x4a4+2(x2y2a2b2)+y4b4]

=

2(x2a4+y2b4)+2(x4a6+x2y2a4b2+x2y2a2b4+y4b6)+(a2+b2)a2b2(x4a4+2x2y2a2b2+y4b4)

(x2a4+y2b4)

=

(x4a6+x2y2a4b2+x2y2a2b4+y4b6)

x2a4+y2b4

=

x4a6+y4b6+x2y2(a2+b2)a4b4

x4b6+y4a6

=

a2b2[x2b4(a2+b2)x2y2+y2a4]

 

=

a2b2[x4b4(a2+b2)x2y2+y4a4]+a2b2[x2b4+y2a4]a2b2[x4b4+y4a4]


Keeping in mind that,

Ψ

=

Ψ0(ρρc)q,

and that, after setting q=3, we have chosen,

FB(Ψ)

=

D1Ψ2/3+D2Ψ

 

=

D1Ψ02/3(ρρc)2+D2Ψ0(ρρc)3,

let's try again.

[(ζ+2Ω)×𝐮]q=3FB(Ψ)

=

6Ψ0{2Ωfρc(ρρc)12Ψ0ρc2[x2a4+y2b4](ρρc)+6Ψ0ρc2(1a2+1b2)(ρρc)2}f^

 

 

+[2D1Ψ02/3(ρρc)+3D2Ψ0(ρρc)2](x2a2+y2b2)

 

=

3Ψ0{2Ωfρc12Ψ0ρc2[x2a4+y2b4]+6Ψ0ρc2(1a2+1b2)(ρρc)}2(ρρc)f^

 

 

+[2D1Ψ02/3+3D2Ψ0(ρρc)]2(ρρc)f^.

Now, set …

2D1Ψ02/3

=

6Ψ0Ωfρc

D1

=

3Ψ01/3Ωfρc;

and, set …

3D2Ψ0

=

18Ψ02(a2+b2)ρc2a2b2

D2

=

6Ψ0(a2+b2)ρc2a2b2.

We then have,

[(ζ+2Ω)×𝐮]q=3FB(Ψ)

=

3Ψ0{12Ψ0ρc2[x2a4+y2b4]}2(ρρc)f^

 

=

72Ψ02ρc2[x2a4+y2b4](ρρc)f^.

 

=

(𝐮𝐮)(ρρc).

VERY INTERESTING! (29 September 2020)

Exponent q = 4

[(ζ+2Ω)×𝐮]q=4

=

8Ψ0[ı^(xa2)+ȷ^(yb2)](ρρc)2{2Ωfρc+8Ψ0ρc2(ρρc)[(ρρc)(1a2+1b2)4(x2a4)4(y2b4)]}.

Trial #4

We begin with the,

Euler Equation
written in terms of the Vorticity and
as viewed from a Rotating Reference Frame

𝐮t+(ζ+2Ωf)×𝐮=1ρP[Φ+12u212|Ωf×x|2] .

Next, we rewrite this expression to incorporate the following three realizations:

  • For a barotropic fluid, the term involving the pressure gradient can be replaced with a term involving the enthalpy via the relation, H=P/ρ.
  • The expression for the centrifugal potential can be rewritten as, 12|Ωf×x|2=12Ωf2(x2+y2).
  • In steady state, 𝐮/t=0.

This means that,

(ζ+2Ωf)×𝐮

=

[H+Φgrav+12u212Ωf2(x2+y2)].

If the term on the left-hand-side of this equation can be expressed in terms of the gradient of a scalar function, then it can be readily grouped with all the other terms on the right-hand-side, which already are in the gradient form.

Building on the insight that we have gained from the above examination of systems for which the exponent, q = 3, let's change the 12u2 term on the RHS to 12(ρu)2 then reexamine the LHS.

[(ζ+2Ωf)×𝐮]q=3

=

[H+Φgrav12Ωf2(x2+y2)][12u2]

 

=

[H+Φgrav12Ωf2(x2+y2)](ρρc)2{(ρρc)2[12u2]}

 

=

[H+Φgrav12Ωf2(x2+y2)](ρρc)2{[12(ρρc)2u2]12u2[(ρρc)2]}

[(ζ+2Ωf)×𝐮]q=3FB

=

[H+Φgrav+FB12Ωf2(x2+y2)](ρρc)2{[12(ρρc)2u2]12u2[(ρρc)2]}.

Now, rewriting the LHS gives,

[(ζ+2Ωf)×𝐮]q=3FB

=

3Ψ0{2Ωfρc12Ψ0ρc2[x2a4+y2b4]+6Ψ0ρc2(1a2+1b2)(ρρc)}2(ρρc)f^

 

 

+{2D1Ψ02/3+3D2Ψ0(ρρc)}2(ρρc)f^

 

=

3Ψ0{12Ψ0ρc2[x2a4+y2b4]}2(ρρc)f^

 

=

36Ψ02ρc2[x2a4+y2b4](ρρc)2,

where we have set,

D1=3Ψ01/3Ωfρc

      and,      

D2=6Ψ0(a2+b2)ρc2a2b2.

Notice that when the exponent, q=3, we have,

[𝐮𝐮]q=3

=

1ρ2{[(ρρc)q1(2qΨ0yb2)]2+[(ρρc)q1(2qΨ0xa2)]2}q=3

 

=

1ρ2{[(ρρc)2(6Ψ0yb2)]2+[(ρρc)2(6Ψ0xa2)]2}

 

=

36Ψ02ρc2(ρρc)2[x2a4+y2b4].

Hence,

[(ζ+2Ωf)×𝐮]q=3FB

=

(ρρc)2u2(ρρc)2.

Trial#5

Let's return to the above-mentioned,

Eulerian Representation
of the Euler Equation
as viewed from a Rotating Reference Frame

𝐮t+(𝐮)𝐮=1ρPΦgravΩf×(Ωf×x)2Ωf×𝐮.

In steady state, this can be rewritten as,

(𝐮)𝐮+2Ωf×𝐮

=

[H+Φgrav12|Ωf×x|2].

Let's focus on the left-hand-side, which is expressed entirely in terms of the rotating-frame velocity, 𝐮, and the (constant) angular frequency of rotation of the coordinate frame, Ωf. Rewriting the LHS, we have,

LHS:     2Ωf×𝐮+(𝐮)𝐮

=

2Ωf[ȷ^uxı^uy]+[uxx+uyy][ı^ux+ȷ^uy]

 

=

2Ωf[ȷ^uxı^uy]+ı^[uxuxx+uyuxy]+ȷ^[uxuyx+uyuyy]

 

=

2Ωf[ȷ^uxı^uy]+[ı^uxuxx+ȷ^uyuyy]+[ı^uyuxy+ȷ^uxuyx]

 

=

2Ωf[ȷ^uxı^uy]+12{[ı^ux2x+ȷ^uy2y]+[ı^uy2x+ȷ^ux2y]}+[ı^uyuxy+ȷ^uxuyx]12[ı^uy2x+ȷ^ux2y]

 

=

2Ωf[ȷ^uxı^uy]+12u2+ı^uy[uxyuyx]+ȷ^ux[uyxuxy].

Next, to the extent possible, let's express the LHS in terms of the dimensionless mass density,

σρρc

=

1(x2a2+y2b2).

We will assume that the stream-function,

Ψ

=

Ψ0σq,

in which case,

ρcσ𝐮

=

ı^Ψyȷ^Ψx

ρc𝐮

=

q(q1)[ı^σq1yȷ^σq1x].

That is,

ρcux

=

q(q1)(σq1y)

      and,      

ρcuy

=

q(q1)(σq1x).

The first term on the LHS becomes,

2Ωf[ȷ^uxı^uy]

=

2Ωfρcqq1[ȷ^(σq1y)+ı^(σq1x)]

 

=

2Ωfρcqq1(σq1).

The third term on the LHS becomes,

ı^uy[uxyuyx]

=

ı^(uyρc){y[q(q1)(σq1y)]+x[q(q1)(σq1x)]}

 

=

q(q1)ı^(uyρc){2σq1}

 

=

[qρc(q1)]2{2σq1ı^(σq1x)}

Similarly, the fourth term on the LHS becomes,

ȷ^ux[uyxuxy]

=

ȷ^(uxρc){x[q(q1)(σq1x)]+y[q(q1)(σq1y)]}

 

=

q(q1)ȷ^(uxρc){2σq1}

 

=

[qρc(q1)]2{2σq1ȷ^(σq1y)}.

Note that,

σq1xi

=

(q1)σq2σxi=(q1)σq2(2xiai2)

(ρcu)2=ρc2(ux2+uy2)

=

q2(q1)2{[(q1)σq2(2xa2)]2+[(q1)σq2(2yb2)]2}

 

=

4q2σ2(q2)[x2a4+y2b4].


Hence,

2σq1

=

x[σq1x]+y[σq1y]

 

=

(q1){x[σq2(2xa2)]+y[σq2(2yb2)]}

 

=

(q1){σq2x[(2xa2)]+(2xa2)x[σq2]+σq2y[(2yb2)]+(2yb2)y[σq2]}

 

=

(q1){[2a2+2b2]σq2+2x(q2)a2[σq3σx]+2y(q2)b2[σq3σy]}

 

=

(q1){[2a2+2b2]σq22(q2)σq3[2x2a4+2y2b4]}.

So, when they are added together, the third and fourth terms give,

ı^uy[uxyuyx]+ȷ^ux[uyxuxy]

=

[qρc(q1)]22σq1{ı^(σq1x)+ȷ^(σq1y)}

 

=

[2q2ρc2(q1)]{[1a2+1b2]σq22(q2)σq3[x2a4+y2b4]}{ı^(σq1x)+ȷ^(σq1y)}

 

=

[2q2ρc2(q1)][1a2+1b2]{σq2}{ı^(σq1x)+ȷ^(σq1y)}

 

 

[4(q2)q2ρc2(q1)]{[(ρcu)24q2]σ1q}{ı^(σq1x)+ȷ^(σq1y)}

 

=

2q2ρc2(2q3)[1a2+1b2]σ2q3(q2)(ρcu)2ρc2ln(σ).

Hence,

LHS:     2Ωf×𝐮+(𝐮)𝐮

=

2qΩfρc(q1)(σq1)+12u2+2q2ρc2(2q3)[1a2+1b2]σ2q3(q2)u2ln(σ).

Note that,

12u2(q2)u2ln(σ)

=

12{u2u2ln[σ2(q2)]}

 

=

u22{ln[u2]ln[σ2(q2)]}

 

=

u22{ln[u2σ2(q2)]}

 

=

u22{ln[(2qρc)2(x2a4+y2b4)]}

 

=

2q2ρc2σ2(q2)[x2a4+y2b4]{ln[(2qρc)2(x2a4+y2b4)]}

 

=

σ2(q2)2{[(2qρc)2(x2a4+y2b4)]}.

Or,

12u2+(2q)u2ln(σ)

=

12{u2+u2ln[σ2(2q)]}

 

=

(12)σ2(2q){σ2(2q)u2+u2[σ2(2q)]}

 

=

(12)σ2(q2){[u2σ2(2q)]}.

Exponent q = 2

LHS:     [2Ωf×𝐮+(𝐮)𝐮]q=2

=

4Ωfρcσ+12u2+8ρc2[1a2+1b2]σ.

Exponent q = 3

LHS:     [2Ωf×𝐮+(𝐮)𝐮]q=3

=

3Ωfρcσ2+12u2+6ρc2[1a2+1b2]σ3u2ln(σ).

 

=

3Ωfρcσ2+6ρc2[1a2+1b2]σ3+u2ln(uσ).

Trial #6

LHS:     2Ωf×𝐮+(𝐮)𝐮

=

2Ωf[ȷ^uxı^uy]+12u2+ı^uy[uxyuyx]+ȷ^ux[uyxuxy].

We will assume that the stream-function,

Ψ

=

Ψ0(ασ)q

Ψxi

=

Ψ0q(ασ)q1σxi,

in which case,

ρcσ𝐮

=

ı^Ψyȷ^Ψx

 

=

ı^Ψ0q(ασ)q1σy+ȷ^Ψ0q(ασ)q1σx

ρc𝐮

=

ı^[Ψ0q(ασ)q1σ]σy+ȷ^[Ψ0q(ασ)q1σ]σx.

That is,

ρcux

=

[Ψ0q(ασ)q1σ]2yb2

      and,      

ρcuy

=

[Ψ0q(ασ)q1σ]2xa2.

The first term on the LHS becomes,

2Ωf[ȷ^uxı^uy]

=

2Ωfρc[Ψ0q(ασ)q1σ][ȷ^(2yb2)+ı^(2xa2)]

 

=

+2Ωfρc[Ψ0q(ασ)q1σ]σ.

Trial #7

Uncluttered Setup

Let's simply look at the vortensity expression as defined in Part II, above, namely,

g(Ψ)

(2Ωf+ζz)ρcσ,

and recognize that we are ultimately interested in the function, FB(Ψ), defined such that,

dFB(Ψ)dΨ

=

g(Ψ).

We start with the expression for the z-component of the vorticity,

ζz

=

x[1ρΨx]y[1ρΨy]

 

=

{x[(Ψ0ρcσ)σqx]+y[(Ψ0ρcσ)σqy]}.

Next, appreciate that,

1σσqxi

=

qσq2σxi

=

(qq1)σq1xi.

Hence,

ζz

=

qΨ0ρc(q1){x[σq1x]+y[σq1y]}

 

=

[qΨ0ρc(q1)]2σq1.

So, the vortensity is,

g(σ)=(2Ωf+ζz)ρcσ

=

(2Ωfρc)σ1[qΨ0ρc2(q1)]σ12σq1.

Let's switch to the stream-function via the assumed relation,

σ

=

(ΨΨ0)1/q;

g(Ψ)

=

(2Ωfρc)(ΨΨ0)1/q[qΨ0ρc2(q1)](ΨΨ0)1/q2(ΨΨ0)(q1)/q.

This expression gives the vortensity in what appears to be the desired form — that is, expressed strictly in terms of the stream function, Ψ — for a wide range of values of the exponent, q. [CAUTION:   the 2 operator is an exception.] It is not yet (13 October 2020) clear to me how — or if — the second term on the right-hand-side of this expression can be integrated to give F(Ψ). But the first term can be obtained from,

F1st(Ψ)

=

(2Ωfρc)q(q1)(ΨΨ0)(q1)/q

dF1st(Ψ)dΨ

=

(2Ωfρc)(ΨΨ0)1/q.

T5 Coordinates

Let's evaluate the 2 operator by expressing it and its argument in terms of T5 Coordinates. Note that,

λ1

(x2+κ2y2)1/2,

where, κa/b. The specified density distribution is, therefore,

σρρc

=

1λ12a2,

and the stream-function is,

ΨΨ0

=

σq=[1λ12a2]q.

The relevant T5-Coordinate System Laplacian is,

2𝔉

=

[1λ122][2𝔉λ12][1λ132]𝔉λ1+[(1+κ2)λ1]𝔉λ1,

where,

(x2+κ4y2)1/2,

and in the present context,

𝔉

=

(ΨΨ0)(q1)/q=[1λ12a2]q1.

Hence,

𝔉λ1

=

2(q1)λ1a2[1λ12a2]q2=[2(q1)λ1a2](ΨΨ0)(q2)/q;

2𝔉λ12

=

2(q1)a2[1λ12a2]q2+2(q1)λ1a2[1λ12a2]q3[2(q2)λ1a2]

 

=

2(q1)a2(ΨΨ0)(q2)/q+4(q1)(q2)λ12a4(ΨΨ0)(q3)/q.

And,

2𝔉

=

[1λ122]{2(q1)a2(ΨΨ0)(q2)/q+4(q1)(q2)λ12a4(ΨΨ0)(q3)/q}

 

 

[1λ132]{[2(q1)λ1a2](ΨΨ0)(q2)/q}+[(1+κ2)λ1]{[2(q1)λ1a2](ΨΨ0)(q2)/q}

 

=

4(q1)(q2)a42(ΨΨ0)(q3)/q[2(q1)(1+κ2)a2](ΨΨ0)(q2)/q.

All Together

Putting this all together, we obtain,

g(Ψ)

=

(2Ωfρc)(ΨΨ0)1/q[qΨ0ρc2(q1)](ΨΨ0)1/q{4(q1)(q2)a42(ΨΨ0)(q3)/q[2(q1)(1+κ2)a2](ΨΨ0)(q2)/q}

 

=

(2Ωfρc)(ΨΨ0)1/q+[2q(1+κ2)Ψ0ρc2a2](ΨΨ0)(q3)/q[4q(q2)Ψ0ρc2a4](x2+κ4y2)(ΨΨ0)(q4)/q.

Note that, for the specific example case of κ2=2,

[12]κ2=2=(x2+4y2)

=

x2Λ=Λλ222[Λ1]=2λ12[ΛΛ+1].

where,

Λ

[1+4λ12λ22]1/2.

See Also

  • Related discussions of models viewed from a rotating reference frame:
Tiled Menu

Appendices: | VisTrailsEquations | VisTrailsVariables | References | Ramblings | VisTrailsImages | myphys.lsu | ADS |