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Jupiter atmospheric dynamics from ground-based

Doppler imaging

François-Xavier Schmider, Ivan Gonçalves, Tristan Guillot, Jason Jackiewicz,

Thomas Underwood, Patrick Gaulme, David Voelz, Thierry Appourchaux,

Patrick Boumier, Raùl Morales-Juberias, et al.

To cite this version:

François-Xavier Schmider, Ivan Gonçalves, Tristan Guillot, Jason Jackiewicz, Thomas Underwood, et

al.. Jupiter atmospheric dynamics from ground-based Doppler imaging. EPSC-DPS Joint Meeting

2019, Sep 2019, Genève, Switzerland. pp.EPSC-DPS2019-1613-2. �hal-03007356�

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Jupiter atmospheric dynamics from ground-based Doppler

imaging

François-Xavier Schmider (1), Ivan Gonçalves (1), Tristan Guillot (1), Jason Jackiewicz (2), Tom Underwood (2), Patrick Gaulme (2,4), David Voelz (2), Thierry Appourchaux (3), Patrick Boumier (3), Raúl Morales-Juberias (5) , Masahiro Ikoma (6), Bun’ei Sato (7) and Hideyuki Iziumura (8)

(1) Université Côte d’Azur, Observatoire de la Cote d’Azur, Lagrange, Nice, France (2) New Mexico State University, NM, USA, (3) Institut d’Astrophysique Spatiale, Orsay, France, (4) Max-Planck-Institut fur Sonnensystemforshung, Göttingen, Germany, (5) New Mexico Institute of Mining and Technology, NM, USA (6) University of Tokyo, Tokyo, Japan, (7) Tokyo Institute of Technology, Tokyo, Japan, (8) Okayama Branch Office, Subaru Telescope, NAOJ, NINS, Okayama, Japan (schmider@oca.eu)

Abstract

The JOVIAL/JIVE project aims at measuring mo-tions at the surface of gaseous planets and to de-tect their acoustic oscillations using a series of dedi-cated Doppler spectro-imagers. The instruments de-tect small Doppler shifts of a set of optical solar lines reflected by the top of the giant planets clouds to in-fer the projected velocity at each point of the plane-tary surface. We focus here on retrieving new infor-mation on atmospheric dynamics of the giant planets and show how planetary rotation can be used to re-construct velocity maps from ground-based observa-tions [2]. Based on observaobserva-tions of Jupiter performed in 2018 at the Dunn Solar Telescope, we provide for the first time a Doppler zonal velocity map including longitudinal structure such as the Great Red Spot. We show that the method can provide vertical and merid-ional circulation as well. Preliminary analysis points to detectable vertical motion at the limit between the equatorial belts and the tropical zones of Jupiter.

1. Introduction

The atmosphere of giant planets, and in particular of Jupiter, is subject to strong winds and huge dynami-cal processes. Juno has revealed new behavior about this dynamics, and in particular the fact that the zonal flow observed by cloud-tracking and the asymmetry between the Northern and Southern hemispheres ex-tends to about 3000 km depth [4]; [3]. However, cloud-tracking can only give a 2D view of the motion at the surface, and can be biased by the presence of waves controlling the shape of the clouds. Doppler spectroscopic measurements can reveal complemen-tary components of the winds, in particular by

provid-ing the velocity along the line-of-sight. Such observa-tions are very difficult both to measure and to interpret. In this presentation, we will summarize the observa-tions that were conducted with a dedicated Doppler imaging instrument (JIVE-JOVIAL) and the main re-sults that were obtained after a careful data processing. We will in particular present maps of zonal and verti-cal components of the winds.

2. Observations

In paper [2], we explained the principle of the JOVIAL Doppler imager and described its performances on ob-servations carried out of Jupiter in 2016 and 2017. In the present paper, we use observations obtained with the same instrument at the Dunn Solar Telescope at Sunspot, New Mexico, between May 4th and May 30th, 2018. A total of 110 hours were obtained over 16 nights. Unlike previous observations, the seeing qual-ity was quite good, 1 arcsec in average. The calibration and data processing is described in [2]. One improve-ment of the measureimprove-ments came from the telescope configuration [5] where the whole focus room can ro-tate around the azimuthal axis, allowing us to take im-ages with different orientations of the instrument in or-der to calibrate the instrumental effects linked to the alignment of the images on the detector.

2.1. Reconstruction of the 2D maps

In the previous work, we mainly derived a zonal wind profile from the individual velocity images. Here, we tried to reconstruct full velocity maps on planispheres. In order to do so, we first corrected the Doppler im-ages from the effect of the PSF, as explained in [1]. We use then the projection factor corresponding to

EPSC Abstracts

Vol. 13, EPSC-DPS2019-1613-2, 2019

EPSC-DPS Joint Meeting 2019

c

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the different components of the wind to deproject the Doppler data onto a planisphere of Jupiter. In princi-ple, Doppler images are insensitive to zonal velocities on the central meridian of the planet, as the motion is perpendicular to the line-of-sight at that location. Due to Jupiter’s rotation over the course of one night, each image corresponds to a different central longitude on Jupiter, and therefore will be projected on the map at different positions and averaged together. At a given longitude of the planisphere, many different images will be averaged with a weight corresponding to their SNR. This results in a complete planisphere for each velocity components. The meridional component is still affected with a high noise level near the equator, as all observations are obtained from the Earth, almost in the equatorial plane. To the contrary, the vertical component is well recovered around the equator.

2.2. Results

We display here the zonal component map. A com-parison was made with OPAL observations of Jupiter with HST, obtained at the same epoch. The zonal map is very similar to what can be obtained from cloud-tracking. In [2], we noticed a lower velocity in the north of the Equatorial Zone. In these new measure-ments, we still observe a reduction of the velocity in this region, but smaller. We see the presence of the Great Red Spot, which is visible as a shear in the zonal velocity above and below the GRS. After removal of the systematics errors, the noise level on the map is of the order of a few m/s.

We can also produced vertical and meridional com-ponents maps. The vertical component and the merid-ional component maps only differ by a factor depend-ing of the planetocentric latitude [1].We observe a vertical downflow or meridional motion at the limit between the Equatorial Belt and the Tropical Zone. There is no way to distinguish between both compo-nents, as all measurements are obtained in the equa-torial plane. The interpretation of these maps requires complementary measurements as can be obtained by cloud-tracking and careful modeling, before we can conclude on the existence of vertical motion.

3. Summary and conclusion

We have shown that Doppler imaging can provide pre-cise information, complementary to cloud-tracking, about atmospheric dynamics of gaseous planet. In the case of Jupiter, we can produce velocity maps for dif-ferent velocity components by combining images

Figure 1: Map of the zonal component of the wind, ob-tained from 16 nights of observations. The colorscale is in m/s, brighter for prograde velocity (eastward) tained from a complete rotation of the planet. We show a full map of the zonal wind that can be com-pared with cloud-tracking images. The techniques al-low us to study also vertical motions. The observations were limited by the terrestrial atmospheric turbulence. The quality of the results could be improved by us-ing simultaneously an Adapted Optics system, which will be developed for that purpose. Ultimately, a ded-icated space mission around the planet would provide much more precise data and would allow to recover the whole dynamical structure.

Acknowledgements

This work was possible thanks to the ANR JOVIAL and the JIVE in NM NASA EPSCOR programme. Ivan Gonçalves was supported by OCA.

References

[1] Gaulme, P., Schmider, F.-X., Gonçalves, I., (2018) Measuring planetary atmospheric dynamics with Doppler spectroscopy, A&A, 617, A41

[2] Gonçalves, I., Schmider, F. X. et al, (2019) First measurements of Jupiter’s zonal winds with visi-ble imaging spectroscopy, Icarus, 319, 795 [3] Guillot, T., et al, (2018) A suppression of

differen-tial rotation in Jupiter’s deep interior, Nature, 555, 227

[4] Kaspi, Y. et al, (2018) Jupiter’s atmospheric jet streams extend thousands of kilometres deep, Na-ture, 555, 223

[5] Underwood, T. A. et al, (2017) Adaptation of Dunn Solar Telescope for Jovian Doppler spectro imaging, SPIE Conference Series, 104010Y

Figure

Figure 1: Map of the zonal component of the wind, ob- ob-tained from 16 nights of observations

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