PGE/RotatingFrame

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NOTE to Eric Hirschmann & David Neilsen... I have move the earlier contents of this page to a new Wiki location called Compressible Riemann Ellipsoids.

Rotating Reference Frame

At times, it can be useful to view the motion of a fluid from a frame of reference that is rotating with a uniform (i.e., time-independent) angular velocity Ωf. In order to transform any one of the principal governing equations from the inertial reference frame to such a rotating reference frame, we must specify the orientation as well as the magnitude of the angular velocity vector about which the frame is spinning, Ω→f; and the d/dt operator, which denotes Lagrangian time-differentiation in the inertial frame, must everywhere be replaced as follows:

[ddt]inertial→[ddt]rot+Ω→f×.

Performing this transformation implies, for example, that

v→inertial=v→rot+Ω→f×x→,

and,

[dv→dt]inertial=[dv→dt]rot+2Ω→f×v→rot+Ω→f×(Ω→f×x→)

=[dv→dt]rot+2Ω→f×v→rot−12∇[|Ω→f×x→|2]

(If we were to allow Ω→f to be a function of time, an additional term involving the time-derivative of Ω→f also would appear on the right-hand-side of these last expressions; see, for example, Eq.~1D-42 in BT87.) Note as well that the relationship between the fluid vorticity in the two frames is,

[ζ→]inertial=[ζ→]rot+2Ω→f.


Continuity Equation (rotating frame)

Applying these transformations to the standard, inertial-frame representations of the continuity equation presented elsewhere, we obtain the:

Lagrangian Representation
of the Continuity Equation
as viewed from a Rotating Reference Frame

[dρdt]rot+ρ∇⋅v→rot=0 ;


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

[∂ρ∂t]rot+∇⋅(ρv→rot)=0 .


Euler Equation (rotating frame)

Applying these transformations to the standard, inertial-frame representations of the Euler equation presented elsewhere, we obtain the:

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

[dv→dt]rot=−1ρ∇P−∇Φ−2Ω→f×v→rot−Ω→f×(Ω→f×x→) ;


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

[∂v→∂t]rot+(v→rot⋅∇)v→rot=−1ρ∇P−∇[Φ−12|Ω→f×x→|2]−2Ω→f×v→rot ;


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

[∂v→∂t]rot+(ζ→rot+2Ω→f)×v→rot=−1ρ∇P−∇[Φ+12vrot2−12|Ω→f×x→|2] .


Centrifugal and Coriolis Accelerations

Following along the lines of the discussion presented in Appendix 1.D, §3 of BT87, in a rotating reference frame the Lagrangian representation of the Euler equation may be written in the form,

[dv→dt]rot=−1ρ∇P−∇Φ+a→fict,

where,

a→fict≡−2Ω→f×v→rot−Ω→f×(Ω→f×x→).

So, as viewed from a rotating frame of reference, material moves as if it were subject to two fictitious accelerations which traditionally are referred to as the,

Coriolis Acceleration

a→Coriolis≡−2Ω→f×v→rot,

(see the related Wikipedia discussion) and the

Centrifugal Acceleration

a→Centrifugal≡−Ω→f×(Ω→f×x→)=12∇[|Ω→f×x→|2]

(see the related Wikipedia discussion).

Nonlinear Velocity Cross-Product

In some contexts — for example, our discussion of Riemann ellipsoids or the analysis by Korycansky & Papaloizou (1996) of nonaxisymmetric disk structures — it proves useful to isolate and analyze the term in the "vorticity formulation" of the Euler equation that involves a nonlinear cross-product of the rotating-frame velocity vector, namely,

A→≡(ζ→rot+2Ω→f)×v→rot.

NOTE: To simplify notation, for most of the remainder of this subsection we will drop the subscript "rot" on both the velocity and vorticity vectors.

Align Ω→f with z-axis

Without loss of generality we can set Ω→f=k^Ωf, that is, we can align the frame rotation axis with the z-axis of a Cartesian coordinate system. The Cartesian components of A→ are then,

i^:Ax=ζyvz−(ζz+2Ω)vy,

j^:Ay=(ζz+2Ω)vx−ζxvz,

k^:Az=ζxvy−ζyvx,

where it is understood that the three Cartesian components of the vorticity vector are,

ζx=[∂vz∂y−∂vy∂z],ζy=[∂vx∂z−∂vz∂x],ζz=[∂vy∂x−∂vx∂y].

In turn, the curl of A→ has the following three Cartesian components:

i^:[∇×A→]x=∂∂y[ζxvy−ζyvx]−∂∂z[(ζz+2Ω)vx−ζxvz],

j^:[∇×A→]y=∂∂z[ζyvz−(ζz+2Ω)vy]−∂∂x[ζxvy−ζyvx],

k^:[∇×A→]z=∂∂x[(ζz+2Ω)vx−ζxvz]−∂∂y[ζyvz−(ζz+2Ω)vy].

When vz=0

If we restrict our discussion to configurations that exhibit only planar flows — that is, systems in which vz=0 — then the Cartesian components of A→ and ∇×A→ simplify somewhat to give, respectively,

i^:Ax=−(ζz+2Ω)vy,

j^:Ay=(ζz+2Ω)vx,

k^:Az=ζxvy−ζyvx,

and,

i^:[∇×A→]x=∂∂y[ζxvy−ζyvx]−∂∂z[(ζz+2Ω)vx],

j^:[∇×A→]y=−∂∂z[(ζz+2Ω)vy]−∂∂x[ζxvy−ζyvx],

k^:[∇×A→]z=∂∂x[(ζz+2Ω)vx]+∂∂y[(ζz+2Ω)vy],

where, in this case, the three Cartesian components of the vorticity vector are,

ζx=−∂vy∂z,ζy=∂vx∂z,ζz=[∂vy∂x−∂vx∂y].

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