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Redalyc.On a Possible Connection Between Chandler Wobble and Dark Brazilian Journal of Physics ISSN: 0103-9733 [email protected] Sociedade Brasileira de Física Brasil Portilho, Oyanarte On a possible connection between Chandler wobble and dark matter Brazilian Journal of Physics, vol. 39, núm. 1, marzo, 2009, pp. 1-11 Sociedade Brasileira de Física Sâo Paulo, Brasil Available in: http://www.redalyc.org/articulo.oa?id=46413555001 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Brazilian Journal of Physics, vol. 39, no. 1, March, 2009 1 On a possible connection between Chandler wobble and dark matter Oyanarte Portilho∗ Instituto de F´ısica, Universidade de Bras´ılia, 70919-970 Bras´ılia–DF, Brazil (Received on 17 july, 2007) Chandler wobble excitation and damping, one of the open problems in geophysics, is treated as a consequence in part of the interaction between Earth and a hypothetical oblate ellipsoid made of dark matter. The physical and geometrical parameters of such an ellipsoid and the interacting torque strength is calculated in such a way to reproduce the Chandler wobble component of the polar motion in several epochs, available in the literature. It is also examined the consequences upon the geomagnetic field dynamo and generation of heat in the Earth outer core. Keywords: Chandler wobble; Polar motion; Dark matter. 1. INTRODUCTION ence of a DM halo centered in the Sun and its influence upon the motion of planets; numerical simulations due to Diemand et al. [8] show the presence of DM clumps surviving near A 305-day Earth free precession was predicted by Euler in the solar circle; Adler [9] suggests that internal heat produc- the 18th century and was sought since then by astronomers in tion in Neptune and hot-Jupiter exoplanets is due to accretion the form of small latitude variations. F. Kustner¨ in 1888 and of planet-bound, not self-annihilating DM. Although the na- S. C. Chandler in 1891 detected such a motion but with a pe- ture of the particles that form DM is not known precisely (see riod of approximately 435 days. Later it was shown by Love for instance Khalil and Munoz˜ [10]) we assume that, as usual, [1] and Larmor [2] that such a disagreement between theory those particles do not interact with regular matter through elec- and observation is in part consequence of elastic deformation tromagnetic force but only gravitationally. Furthermore, we of the Earth which was not considered by the Euler rigid body speculate that they can interact with each other in such a way model (see Smith and Dahlen [3] for further corrections expla- to set up an oblate (due to rotation) ellipsoid that might be nation). The so called Chandler wobble (CW) is actually one present inside Earth, occupying the same space without violat- of the major components of the Earth polar motion, together ing any physical law. It can be shown that such an ellipsoid, with the annual wobble (AW) which has period of nearly 365 made of self-interacting DM (otherwise such a structure would days. The composition of the two wobbles results in a motion not be possible), would be attached to Earth through a spring- with period of around 6.2 years due to the beat phenomenon. like restoring force. In this line, excitation and damping of CW The ever increasing measurement precision, for which tech- could be, at least partially, consequence of energy exchange niques like very long baseline interferometry (VLBI), global between the two bodies, associated to the restoring torque be- positioning system (GPS) and lunar laser ranging (LLR) are tween them. The model does not consider the other known employed today, has lead to the conclusion that both wobbles sources for the process nor the Earth internal structure, what have varying amplitudes. For AW, this may be attributed to are of course over simplifications. However this becomes pos- seasonal displacement of atmospheric and water masses. On sible a simple starting point for the calculations, to be sophis- the other hand, excitation and damping of the Chandler wob- ticated in a later step. Hopfner¨ [11, 12] has managed to iso- ble has become a puzzle to investigators. Several mechanisms late the CW and AW components from available polar motion have been proposed for its excitation like snow, hidrological, data. Our goal is to reproduce Hopfner’s¨ results for Chandler atmospheric and oceanic mass displacements, and large earth- wobble in various epochs by adjusting the unknown physical quakes, with defenders and opponents arguing for and against and geometrical parameters of the dark matter ellipsoid. For repeatedly and, in view of the large energy involved, the prob- this purpose, we describe both body motion by solving numer- lem is still an open question. In more recent papers, Gross ically the set of differential equations that emerge from Euler [4] attributes the excitation to ocean bottom pressure variations equations and demonstrate that CW can be reproduced in such and changes in ocean currents due to winds while Seitz et al. manner. This is explained in the next section while results and [5] focus on combined effects due to atmospheric and oceanic discussion are presented in section III. causes. Since it is believed that dark matter (DM) and dark energy composes around 96% of the mass of the Universe we investi- gate in this paper the possibility of DM to contribute, at least 2. THE MODEL in part, for the excitation and damping of Chandler wobble. The effect of DM upon regular matter has been considered We start by calculating the torque that arises when the polar mainly on galactic-scale although more recently some authors principal axes 3 and 3∗ of two oblate ellipsoids with isotropic have studied smaller scale effects. For instance, Froggatt and densities interacting through the gravitational force are tilted Nielsen [6]) have investigated the possibility of star-scale ef- by an angle α (see Fig. 1). The gravitational potential at a fects due to small DM balls; Frere` et al. [7] studied the pres- point outside the internal ellipsoid (see e. g. Stacey [13]) is given by ∗ GM G ∗ ∗ ∗ V(r,θ) ≈ − + (C − A )P (cosθ) (1) Electronic address: [email protected] r r3 2 2 Oyanarte Portilho 3* 3 sidering the Earth tilted by an angle α around the 1-axis (Fig. 1) with respect to the internal ellipsoid it suffers therefore a torque given by the integral dm r θ 2 Z α τ = sinφdτ (3) α directed towards the identical axes 1 and 1∗, as projected by 2* φ the presence of sinφ in this integral. The integration should in principle be performed over the entire Earth volume. However considering the Earth density as isotropic, as it is done in the Preliminary Reference Earth Model - PREM (Dziewonski and Anderson [14]), it can be shown that the spherical volume in- 1=1* ternal to the Earth with radius the same as the polar radius does not contribute to the integral. Therefore the integration over r ranges from Rp, the polar radius, to the radius of the geoid at FIG. 1: Two ellipsoids tilted by an angle α around the common equa- a given direction. On the other hand, it is well known (see, for torial principal axes 1 and 1∗. The spherical coordinates (r, θ, φ) instance, Stacey [13]) that the equation of the geoid is written that give the position of an infinitesimal mass dm with respect to the in the first order approximation in terms of the co-latitude θ0 as 1∗2∗3∗ reference frame are also shown. 2 0 rg ≈ a(1 − f cos θ ), (4) neglecting higher order terms. Here M∗, A∗ and C∗ are the mass, equatorial and polar momenta of inertia of the internal where a is the equatorial radius and f = 1−Rp/a is the flatten- 2 ellipsoid, respectively, and P2(cosθ) = (3cos θ − 1)/2 is the ing. Let us write above equation for the case where the geoid Legendre polynomial of second order. The torque over an in- is tilted by an angle α around the 1-axis (Fig. 1), which yields finitesimal mass dm located at that point is then r ≈ a1 − f (cosαcosθ − sinαsinθsinφ)2, (5) ∂V 3G(C∗ − A∗) g dτ = −dm = sin(2θ)dm. (2) ∂θ 2r3 where φ, together with co-latitude θ, is part of the spherical co- and is directed orthogonal to the plane formed by the polar ordinates in the 1∗2∗3∗ reference frame. Therefore the torque principal axis 3∗ and the position r of dm (see Fig. 1). Con- given by equation (3) becomes 3 Z π τ = ρG(C∗ − A∗) dθ sin(2θ)sinθ 2 0 Z 2π a × dφ sinφln 1 − f (cosαcosθ − sinαsinθsinφ)2 , (6) 0 Rp where ρ is the average Earth mass density in that region, taken where A and C are the equatorial and polar momentum of as 2600 kg/m3 [14]. Considering that f = 1/298.257 << 1, inertia of Earth, which is supposed to be axially symmetric we can use the approximation ln(1 + x) ≈ x, obtaining (B = A), ω1, ω2, ω3 are the components of the Earth angu- lar velocity ω in the 123 reference frame, which is attached τ = c sin(2α), (7) 1 to Earth such that the 3-axis coincides with the polar princi- 4π ∗ ∗ pal axis, i. e., the symmetry axis of the oblate ellipsoid, 1- with c1 = 5 ρG(C − A ) f . Notice that this is a restoring ◦ torque when α is around 90 , which gives the stable angular and 2-axis are equatorial principal axes and τ1, τ2 are compo- position if no initial angular momenta were involved.
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