posted on 2022-01-25, 10:57authored bySJ Bolton, S Levin, T Guillot, C Li, Y Kaspi, G Orton, MH Wong, F Oyafuso, M Allison, J Arballo, S Atreya, HN Becker, J Bloxham, S Brown, LN Fletcher, E Galanti, S Gulkis, M Janssen, A Ingersoll, JL Lunine, S Misra, P Steffes, D Stevenson, JH Waite, RK Yadav, Z Zhang
Jupiter’s atmosphere has a system of zones and belts punctuated by small and large vortices, the largest being the Great Red Spot. How these features change with depth is unknown, with theories of their structure ranging from shallow meteorological features to surface expressions of deep-seated convection. We present observations of atmospheric vortices using the Juno spacecraft’s Microwave Radiometer. We found vortex roots that extend deeper than the altitude at which water is expected to condense, and we identified density inversion layers. Our results constrain the three-dimensional structure of Jupiter’s vortices and their extension below the clouds.
Funding
National Aeronautics and Space Administration (NASA)
Centre National d’Etudes Spatiales
Royal Society Research Fellowship and European Research Council Consolidator Grant (under the European Union’s Horizon 2020 research and innovation program, grant agreement 723890)
Israeli Space Agency, the Helen Kimmel Center for Planetary Science at the Weizmann Institute of Science (WIS)
NASA through cooperative agreement 80NSSC19M0189 and Juno Participating Scientist grant 80NSSC19K1265
grants GO-14661 and GO-15665 from the Space Telescope Science Institute, which is operated by AURA under NASA contract NAS 5-26555.
History
Citation
SCIENCE, Vol 374, Issue 6570, pp. 968-972, DOI: 10.1126/science.abf1015
Author affiliation
School of Physics and Astronomy
Version
AM (Accepted Manuscript)
Published in
Science
Volume
374
Issue
6570
Pagination
968 - 972
Publisher
American Association for the Advancement of Science (AAAS)