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Implications of the ammonia distribution on Jupiter from 1 to 100 bars as measured by the Juno microwave radiometer.
Ingersoll, Andrew P; Adumitroaie, Virgil; Allison, Michael D; Atreya, Sushil; Bellotti, Amadeo A; Bolton, Scott J; Brown, Shannon T; Gulkis, Samuel; Janssen, Michael A; Levin, Steven M; Li, Cheng; Li, Liming; Lunine, Jonathan I; Orton, Glenn S; Oyafuso, Fabiano A; Steffes, Paul G.
Afiliação
  • Ingersoll AP; Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA.
  • Adumitroaie V; Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA.
  • Allison MD; Goddard Institute for Space Studies, New York, NY 10025, USA.
  • Atreya S; Climate and Space Sciences, University of Michigan, Ann Arbor, MI 48109, USA.
  • Bellotti AA; Center for Space Technology and Research, Georgia Institute of Technology, Atlanta, GA 30332, USA.
  • Bolton SJ; Southwest Research Institute, San Antonio, TX 78238, USA.
  • Brown ST; Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA.
  • Gulkis S; Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA.
  • Janssen MA; Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA.
  • Levin SM; Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA.
  • Li C; Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA.
  • Li L; Department of Physics, University of Houston, Houston, TX 77004, USA.
  • Lunine JI; Department of Astronomy, Cornell University, Ithaca, NY 14853, USA.
  • Orton GS; Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA.
  • Oyafuso FA; Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA.
  • Steffes PG; Center for Space Technology and Research, Georgia Institute of Technology, Atlanta, GA 30332, USA.
Geophys Res Lett ; 44(15): 7676-7685, 2017 Aug 16.
Article em En | MEDLINE | ID: mdl-33100420
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.
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Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Idioma: En Ano de publicação: 2017 Tipo de documento: Article

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Idioma: En Ano de publicação: 2017 Tipo de documento: Article