A new study suggests that during Jupiter’s violent storms, hailstones form from a cooled mixture of water and ammonia gas, similar to the process in Earth’s storms where hail forms in the presence of supercooled liquid water; growth of these Jovian hailstones, dubbed ‘mushballs,’ creates a slush-like substance surrounded by a layer of ice, and mushballs fall, evaporate, and continue sinking further in the gas giant’s deep atmosphere.
Fig: This image captured by NASA’s Juno orbiter shows a multitude of magnificent, swirling clouds in Jupiter’s North North Temperate Belt. The image was taken at 4:58 p.m. EDT on October 29, 2018 (1:58 p.m. PDT) as the spacecraft performed its 16th close flyby of Jupiter. At the time, Juno was about 4,400 miles (7,000 km) from the planet’s cloud tops, at a latitude of approximately 40 degrees north. Image credit: NASA / JPL-Caltech / SwRI / MSSS / Gerald Eichstaedt / Sean Doran.
NASA’s Juno mission revealed that Jupiter’s atmosphere is much more complex and intriguing than previously anticipated.
Most of the planet’s atmosphere was shown to be depleted — which is to say, missing — in ammonia.
While ammonia was expected to be well mixed, large scale variability of ammonia was detected at least 100 km (62 miles) below the cloud level where condensation occurs.
Dr. Scott Bolton, Juno’s principal investigator at the Southwest Research Institute, Dr. Tristan Guillot, a Juno co-investigator from the Université Côte d’Azur, and their colleagues propose a new mechanism to explain this depletion and variability.
Jupiter’s mushballs get so big, even the updrafts can’t hold them, and they fall deeper into the atmosphere, encountering even warmer temperatures, where they eventually evaporate completely. Their action drags ammonia and water down to deep levels in the planet’s atmosphere.
Fig: This graphic depicts the evolutionary process of ‘shallow lightning’ and ammonia-water mushballs. An anvil-shaped thunderstorm cloud originates about 65 km (40 miles) below Jupiter’s visible cloud deck. Powered by water-based moist convection, the cloud generates strong updrafts that move liquid water and water ice particles upward. About 19 km (12 miles) up, temperatures are so low that all of the water particles turn to ice. Still climbing, the ice particles cross a region located about 23 km (14 miles) below the upper clouds, where temperatures are between minus 85 degrees Celsius (minus 121 degrees Fahrenheit) and minus 100 degrees Celsius (minus 150 degrees Fahrenheit), depicted as green-hashed layer. At that point, ammonia vapor in the atmosphere acts like an antifreeze, melting the water-ice crystals, transforming them into ammonia-water liquid droplets which then grow and gather a solid icy shell to become mushballs. Once big enough, these slushy hailstones fall down, transporting both ammonia and water into Jupiter’s deep atmosphere where the mushballs eventually evaporate. Image credit: NASA / JPL-Caltech / SwRI / CNRS.
That explains why we don’t see much of it in these places with Juno’s Microwave Radiometer.
References: Tristan Guillot David J. Stevenson Sushil K. Atreya Scott J. Bolton Heidi N. Becker, “Storms and the Depletion of Ammonia in Jupiter: I. Microphysics of “Mushballs””, Journal of Geophysical Research: Planets, Volume 125, Issue 8, 2020, doi: https://doi.org/10.1029/2020JE006403