| Issue |
A&A
Volume 706, February 2026
|
|
|---|---|---|
| Article Number | A109 | |
| Number of page(s) | 8 | |
| Section | Planets, planetary systems, and small bodies | |
| DOI | https://doi.org/10.1051/0004-6361/202556819 | |
| Published online | 05 February 2026 | |
Juno radio occultations reveal the structure of Jupiter's cold northern polar vortex
1
Department of Earth and Planetary Sciences, Weizmann Institute of Science,
Rehovot
76100,
Israel
2
School of Physics and Astronomy, University of Leicester,
Leicester,
UK
3
Jet Propulsion Laboratory, California Institute of Technology,
Pasadena,
CA,
USA
4
Department of Industrial Engineering, University of Bologna,
Forlì,
Italy
5
School of Electrical and Computer Engineering, Georgia Institute of Technology,
Atlanta,
GA,
USA
6
Southwest Research Institute,
San Antonio,
TX,
USA
★ Corresponding authors: This email address is being protected from spambots. You need JavaScript enabled to view it.
; This email address is being protected from spambots. You need JavaScript enabled to view it.
Received:
11
August
2025
Accepted:
29
November
2025
Context. Jupiter’s polar upper troposphere and stratosphere host a persistent cold vortex poleward of 65°N, but its detailed structure and dynamics have remained difficult to resolve.
Aims. The goal is to characterize the thermal structure and dynamics of the polar vortex using new and complementary remote sensing techniques.
Methods. We used a combination of high-resolution vertical profiles derived from Juno’s recent radio occultation measurements and mid-infrared imaging from the VLT/VISIR instrument. The former provided direct retrievals of temperature and density near and within the vortex, while VISIR imaging revealed spatial thermal contrasts across the region.
Results. Our analysis confirms the presence of a steep meridional temperature jump at 65°N, of about 7±1 K at 100 mbar, which is consistent with a strong vertical wind shear and a prograde polar stratospheric jet reaching up to 80 ms−1 at the 10 mbar level. We find the atmosphere to be thermally stable above 0.55 bar, reaching a Brunt-Väisälä frequency of 0.025 s−1 in the mid-stratosphere. Thermal contrasts observed in the infrared data align with the vertical structures inferred from radio occultations, which validates the presence and extent of the cold vortex.
Conclusions. These findings offer a quantitative analysis of the thermal structure and the dynamical behavior of Jupiter’s polar atmosphere and demonstrate the diagnostic power of combining radio occultation and thermal infrared techniques in planetary atmospheric studies.
Key words: methods: observational / planets and satellites: atmospheres / planets and satellites: gaseous planets / planets and satellites: individual: Jupiter
© The Authors 2026
Open Access article, published by EDP Sciences, under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
This article is published in open access under the Subscribe to Open model. This email address is being protected from spambots. You need JavaScript enabled to view it. to support open access publication.
Current usage metrics show cumulative count of Article Views (full-text article views including HTML views, PDF and ePub downloads, according to the available data) and Abstracts Views on Vision4Press platform.
Data correspond to usage on the plateform after 2015. The current usage metrics is available 48-96 hours after online publication and is updated daily on week days.
Initial download of the metrics may take a while.