| Literature DB >> 33100420 |
Andrew P Ingersoll1, Virgil Adumitroaie2, Michael D Allison3, Sushil Atreya4, Amadeo A Bellotti5, Scott J Bolton6, Shannon T Brown2, Samuel Gulkis2, Michael A Janssen2, Steven M Levin2, Cheng Li2, Liming Li7, Jonathan I Lunine8, Glenn S Orton2, Fabiano A Oyafuso2, Paul G Steffes5.
Abstract
The latitude-altitude map of ammonia mixing ratio shows an ammonia-rich zone at 0-5°N, with mixing ratios of 320-340 ppm, extending from 40-60 bars up to the ammonia cloud base at 0.7 bars. Ammonia-poor air occupies a belt from 5-20°N. We argue that downdrafts as well as updrafts are needed in the 0-5°N zone to balance the upward ammonia flux. Outside the 0-20°N region, the belt-zone signature is weaker. At latitudes out to ±40°, there is an ammonia-rich layer from cloud base down to 2 bars which we argue is caused by falling precipitation. Below, there is an ammonia-poor layer with a minimum at 6 bars. Unanswered questions include how the ammonia-poor layer is maintained, why the belt-zone structure is barely evident in the ammonia distribution outside 0-20°N, and how the internal heat is transported through the ammonia-poor layer to the ammonia cloud base.Entities:
Keywords: Juno; Jupiter; atmosphere; dynamics; giant planet; microwave
Year: 2017 PMID: 33100420 PMCID: PMC7580824 DOI: 10.1002/2017gl074277
Source DB: PubMed Journal: Geophys Res Lett ISSN: 0094-8276 Impact factor: 4.720