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Using Jupiter’s gravitational field to probe the Jovian convective dynamo

Convective motion in the deep metallic hydrogen region of Jupiter is believed to generate its magnetic field, the strongest in the solar system. The amplitude, structure and depth of the convective motion are unknown. A promising way of probing the Jovian convective dynamo is to measure its effect on the external gravitational field, a task to be soon undertaken by the Juno spacecraft. We calculate the gravitational signature of non-axisymmetric convective motion in the Jovian metallic hydrogen region and show that with sufficiently accurate measurements it can reveal the nature of the deep convection.

Jupiter possesses the strongest planetary magnetic field in the solar system, more than ten times larger than that of Earth 1 . It is widely accepted that the Jovian magnetic field is generated by convection-driven motion in the deep metallic hydrogen region of the planet 2,3 . However, we know very little about the amplitude and structure of the convective motion, and we do not even know the depth at which the Jovian dynamo operates 3 . Magnetohydrodynamic dynamo processes taking place in the Jovian deep interior are highly complex: thermal buoyancy forces in the metallic region drive convective motion which is strongly controlled by Coriolis forces and which, through magnetic induction, converts the mechanical energy of the fluid motion into the ohmic dissipation of the magnetic field. Though progress has been made in modeling the Jovian convective dynamo 4,5 , achieving the realistic physical parameters probably never will be possible and extrapolating the convective dynamo from a numerically accessible model over many orders of magnitude would lead to a high uncertainty. Here we propose that high-precision measurements of the Jovian gravitational field can provide a window into the phenomenon.
Using a fully three-dimensional finite element model we calculate the external gravitational signature of non-axisymmetric motions in the dynamo region of Jupiter's deep interior. Juno, or some future Jupiter orbiter, could measure this signature thereby sounding the deep interior. The model is characterized by the depth H to the top of the dynamo region, the typical horizontal length scale L of the convection and its amplitude U 0 . It assumes that Jupiter is isolated, rotates rapidly about the symmetry axis, and consists of a compressible barotropic fluid (a polytrope of index unity) whose density is a function only of pressure 6,7 . The axisymmetric zonal winds at Jupiter's cloud level are confined in the outer molecular layer with equatorial thickness H and the underlying metallic hydrogen region has equatorial radius (R e − H), where R e is Jupiter's equatorial radius. The Jovian magnetic field is generated by a parameterized convection with amplitude U 0 and horizontal length scale L in the metallic hydrogen region. The horizontal scale L is related to an azimuthal wavenumber m 0 . Although the Jovian magnetic field does not explicitly enter the gravitational sounding model, U 0 and m 0 reflect the properties of the Jovian convective dynamo 8,9 . For example, a small azimuthal wavenumber m 0 = O(1) (large horizontal scale) dominating the structure of the fluid motion could be indicative of a strong field Jovian dynamo with a large invisible toroidal component of the internal field. A large value of m 0 (small horizontal scale) could be indicative of a weak field Jovian dynamo. Additional model details can be found in the Methods section. gravitational field. Because of axisymmetry, the zonal-wind-induced density anomalies only modify the zonal gravitational coefficients 6,10 . The convection-induced gravitational perturbation is non-axisymmetric, and so it can be readily discerned from the gravitational anomalies caused by the fast zonal winds.
We know very little about the typical amplitude U 0 and the spatial structure of the convective motion taking place in the deep interior of Jupiter 3 . It is believed that U 0 would be much smaller than the speed of the fast zonal winds which is of O(100) m/s. Estimates of U 0 in the metallic hydrogen-helium region vary from This uncertainty is because we cannot access the Jovian physical parameters via direct numerical simulation and an extrapolation on the basis of scaling laws over many orders of magnitude is highly unreliable 3,11 . In our current solutions of gravitational sounding, we take the amplitude = . We first consider a solution with a large horizontal scale of the convective flow marked by the azimuthal wavenumber m 0 = 2, which may correspond to a strong field Jovian dynamo. A three-dimensional view of the density anomalies induced by the convective motion in the non-spherical metallic dynamo region with depth parameter H = 0.1R e is shown in Fig. 1(a) and the corresponding radial gravitational anomalies near the outer bounding surface of Jupiter are shown in in Fig. 1(b). It can be seen, as expected, that the density anomalies are also characterized by azimuthal wavenumber m = 2 and have typical amplitude of O(0.01) kg/m 3 . The gravitational anomalies are largely dominated by the two spherical harmonics, Y 2 2 and Y 4 2 and have magnitude O(1) mgal. The convective motions of a weak-field Jovian dynamo in the metallic hydrogen-helium region would have a small horizontal scale 8 . In this case, we expect that the induced external gravitational signature would be weaker even with the same amplitude U 0 because the signature represents a globally average quantity. Accordingly, we carry out a computation for the same amplitude = . U 1 0 0 m/s but with a smaller horizontal scale of flow with azimuthal wavenumber m 0 = 8. A three-dimensional view of the density anomalies in the metallic dynamo region is shown in Fig. 3(a) and the radial gravitational anomalies near the outer bounding surface are depicted in Fig. 3(b) for the depth parameter H = 0.1R e . The density and gravity anomalies are also characterized by m = 8 and have amplitudes O(0.001) kg/m 3 and O(0.1) mgal. The gravitational anomalies have a structure dominated by Y 8 8 and Y 10 8 . A small-scale convective flow produces a weak gravitational signature that would be more difficult to detect.

Discussion
The results reported in this paper have significant implications for interpreting any nonaxisymmetric gravitational field detected by Juno or some future Jupiter orbiter and for understanding the physics of the convection-driven It is anticipated that the ongoing Juno spacecraft will achieve high precision with the expected noise level of O(10 −3 ) mgal and relative uncertainty 10 −9 for acceleration measurements 12,13 . Our gravitational sounding model predicts that nonaxisymmetric convective motion with typical amplitude = U 1 0 m/s produces radial gravitational anomalies with the magnitude O(1) mgal near the outer bounding surface of Jupiter and that non-axisymmetric motion with typical amplitude = . U 0 1 0 m/s produces anomalies with magnitude O(0.1) mgal. An accurate model of three-dimensional gravitational sounding together with detection of a nonaxisymmetric gravitational field will enable an important constraint on the amplitude, structure and location of the convection-driven Jovian dynamo. It is shown that high-precision measurements of the Jovian gravitational field can provide a complementary and effective way of probing the Jovian convective dynamo via three-dimensional gravitational sounding. Although our paper does not deal specifically with Saturn, our theory can also be applied to the gravitational measurements that will be made by the Cassini spacecraft at its end of mission.

Methods
In our model of gravitational sounding, we regard some parameters of Jupiter as being well determined by observations while other parameters are treated as unknown. The equatorial and polar radii of Jupiter R e and R p ,which are R e = 71492 km and R p = 66854 km -and the angular velocity Ω J = 1.7585 × 10 −4 s −1 and the total mass M J = 1.8986 × 10 27 kg will be regarded as known parameters. According to the models of Jupiter 7,14 , its interior, if the small rocky core is neglected, consists of two major parts: the outer molecular insulating envelope where the observed cloud-level zonal winds may be able to penetrate and the metallic hydrogen-helium region where the Jovian magnetic field is generated by its convective dynamo. It is well known that both the outer surface of the molecular envelope and the molecular-metallic interface are, because of rapid rotation and non-uniform density, non-spheroidal. A recent study 15 shows, however, that the assumption of Roberts 16 -that all equidensity surfaces for the hydrostatic equilibrium of a rapidly rotating Jupiter-like gaseous body are in the shape of oblate spheroids whose eccentricities are a function of the equatorial radius and whose axes of symmetry are parallel to the rotation axis-represents a reasonably accurate approximation. Our model assumes that both the molecular-metallic interface and the outer surface of the molecular envelope are in the shape of oblate spheroids with different eccentricities.
Our model also assumes that the Rossby number for the deep convective flow U u 0 with the typical amplitude U 0 is small, viscous forces are much smaller than the Coriolis forces, the planet is rotating rapidly about the symmetry z-axis with the angular velocity Ω  z J and is in a statistically steady state. The assumption leads to the following governing equations in the rotating frame of reference: where U u 0 represents the velocity of convection, r denotes the position vector with origin at the center of figure, p(r) is the pressure and ρ(r) is the density, K is a constant, and V is the gravitational potential with G = 6.67384 × 10 −11 m 3 kg −1 s −2 the universal gravitational constant. Although the effect of Lorentz forces produced by the magnetic field B cannot be explicitly included in the present model, it is implicitly reflected in the structure of the convective flow. According to the well-known magnetohydrodynamic theory for rapidly rotating systems 8,17 , a large horizontal scale of the flow marked by a small azimuthal wavenumber is likely associated with a Jovian dynamo with a strong magnetic field B while a small horizontal scale of the flow marked by a large azimuthal wavenumber is likely related to a Jovian dynamo with a weak magnetic field B.
Eqs (1-4) with a parameterized convective flow U u 0 are to be solved subject to the two boundary conditions = p 0, For a mathematical description of the problem in the non-spherical metallic region, it is convenient to adopt cylindrical polar coordinates (s, φ, z) with s = 0 at the rotation axis of Jupiter, z = 0 at its equatorial plane and the corresponding unit vectors ( φˆŝ z , , ). Eqs (1)(2)(3)(4) are then solved by a perturbation method making use of the expansions φ = + ′ p p s z p s z ( , ) ( , , ), 0 where the leading-order solution, [p 0 (s, z), ρ 0 (s, z), V 0 (s, z)], is two-dimensional and represents a hydrostatic state that accounts for the effect of rotational distortion but unaffected by the convective flow, and the next-order solution, p′ (s, φ, z), ρ′ (s, φ, z) and V′ (s, φ, z), is fully three-dimensional and denotes the perturbations arising from the effect of the deep convection U u 0 . The expansions yield two problems that are mathematically coupled and inseparable. The leading-order problem determines the shape S of Jupiter as well as the internal distribution p 0 (s, z), ρ 0 (s, z) and V 0 (s, z) in the hydrostatic equilibrium while the next-order problem, which is based on the leading-order solution, determines the perturbations p′ (s, φ, z), ρ′ (s, φ, z) and V′ (s, φ, z) caused by the convective flow.
Substitution of the expansions into Eqs (1-4) yields the leading-order problem governed by