2021
DOI: 10.1051/0004-6361/202140330
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First direct measurement of auroral and equatorial jets in the stratosphere of Jupiter

Abstract: Context. The tropospheric wind pattern in Jupiter consists of alternating prograde and retrograde zonal jets with typical velocities of up to 100 m s−1 around the equator. At much higher altitudes, in the ionosphere, strong auroral jets have been discovered with velocities of 1−2 km s−1. There is no such direct measurement in the stratosphere of the planet. Aims. In this Letter, we bridge the altitude gap between these measurements by directly measuring the wind speeds in Jupiter’s stratosphere. Methods. We us… Show more

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Cited by 30 publications
(57 citation statements)
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“…The zonal wind map we obtained from the Gemini/TEXES measurements in March 2017 combined with the 1 mbar zonal wind measured by Cavalié et al (2021) using ALMA and the result obtained by Fletcher et al (2016) from the zonal temperature field measured by IRTF/TEXES in December 2014 are of almost opposite phase in the 1-10 mbar range. The time-interval between the two measurements is ∆T ∼2 yr and 4 months.…”
Section: Zonal Winds In the Jeo Regionmentioning
confidence: 60%
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“…The zonal wind map we obtained from the Gemini/TEXES measurements in March 2017 combined with the 1 mbar zonal wind measured by Cavalié et al (2021) using ALMA and the result obtained by Fletcher et al (2016) from the zonal temperature field measured by IRTF/TEXES in December 2014 are of almost opposite phase in the 1-10 mbar range. The time-interval between the two measurements is ∆T ∼2 yr and 4 months.…”
Section: Zonal Winds In the Jeo Regionmentioning
confidence: 60%
“…-We used the recent and first measurements of the Jovian stratospheric winds obtained from ALMA observations (Cavalié et al 2021), with the temperature field obtained almost simultaneously in March 2017 in the mid-infrared from Gemini/TEXES observations (Giles et al 2020), to derive the zonal wind field as a function of pressure and latitude in the equatorial zone of Jupiter's stratosphere where the Jupiter equatorial oscillation occurs. -We used the thermal wind equation, complemented by the equatorial thermal wind equation of Marcus et al (2019) for the latitudes about the equator, to derive the Jovian stratospheric zonal winds from 0.05 to 30 mbar and from 35 • S to 35 • N. -We derive the absolute stratospheric zonal wind speeds ±35 • about the equator, where the JEO takes place.…”
Section: Discussionmentioning
confidence: 99%
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