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  • American Geophysical Union (AGU)  (2)
  • Atreya, S. K.  (2)
  • 1980-1984  (2)
Material
Publisher
  • American Geophysical Union (AGU)  (2)
Language
Years
  • 1980-1984  (2)
Year
  • 1
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1983
    In:  Journal of Geophysical Research: Space Physics Vol. 88, No. A8 ( 1983-08), p. 6143-6163
    In: Journal of Geophysical Research: Space Physics, American Geophysical Union (AGU), Vol. 88, No. A8 ( 1983-08), p. 6143-6163
    Abstract: Voyager ultraviolet spectrometer (UVS) measurements provided the first unassailable evidence for particle precipitation in the Jovian atmosphere. Strong Lyman and Werner band emissions at high latitudes indicate particle precipitation energy fluxes of about 10 ergs cm −2 s −1 . On the other hand dayglow Lyman and Werner emissions at mid‐ and low‐latitudes may indicate additional particle precipitation fluxes on the order of 0.3 ergs cm −2 s −1 at all latitudes. Such particle precipitation can have significant aeronomical effects on the Jovian thermsophere and ionosphere. A one‐dimensional theoretical model is used to study these effects for the case of electron precipitation, although ion precipitation produces similar effects. Diffusion equations are solved for all the major neutral species and for H + , and photochemical solutions are given for the short lived ions. These neutral and ionospheric components of the model are coupled with the electron and ion energy equations and a two‐stream electron transport code that calculates the energy deposition of precipitating electrons (considered to be the precipitating particles) and photoelectrons. An independent calculation of the vertical neutral temperature is also obtained. The results of the model calculations can be broadly categorized as effects of electron precipitation (1) on the neutral composition and temperature of the thermosphere, and (2) on the composition and structure of the ionosphere. Auroral electron precipitation by 10‐keV electrons with a total energy flux of 10 ergs cm −2 s −1 produces 4.7×10 11 H atoms cm −2 s −1 and 5 ergs cm −2 s −1 of heat, over 2 orders of magnitude larger than solar EUV processes that produce 3.3×10 9 H atoms cm −2 s −1 and 0.03 ergs cm −2 s −1 of heat. Thus, Jovian auroral H production coupled with aurorally driven meridional winds in the thermosphere can possibly explain the high concentration of atomic hydrogen in the low‐latitude Jovian upper atmosphere. Furthermore, aurorally produced changes in composition can create important feedback which affects the relative airglow efficiencies and heating rates in the high‐latitude thermosphere. In addition, ionization and vibrational heating of H 2 from precipitation processes appear to play a central role in determining the structure of the high‐latitude ionosphere. Theoretical fits to the Voyager radio occultation electron density profiles at high latitudes suggest a 10‐keV electron aurora with an energy flux of 10 ergs cm −2 s −1 coupled with a height‐dependent H 2 vibrational temperature that reaches 3000 K in the topside ionosphere.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1983
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  • 2
    Online Resource
    Online Resource
    American Geophysical Union (AGU) ; 1981
    In:  Journal of Geophysical Research: Space Physics Vol. 86, No. A10 ( 1981-09-30), p. 8259-8284
    In: Journal of Geophysical Research: Space Physics, American Geophysical Union (AGU), Vol. 86, No. A10 ( 1981-09-30), p. 8259-8284
    Abstract: The Voyager ultraviolet spectrometers (UVS) have been making almost continuous observations, in the 500‐Å to 1700‐Å wavelength range, of sources in the solar system and galaxy since launch in 1977. Due to their sensitivity, stability, and dynamic range, the spectrometers have made a remarkable number of discoveries pertaining to the Jupiter system, the interstellar medium, astronomical, and astrophysical sources. The most surprising general aspect of these results has been the wide variety of emission processes and species which have been observed. On Jupiter's disc, the emissions detected to date are H Lyman α, H Lyman β, He (584 Å), and the H 2 Lyman and Werner bands. The atomic emissions are excited by resonance scattering of sunlight, while the H 2 bands appear to be excited by particle precipitation. On the nightside disc, only H Lyman α is present. Jupiter's auroral region is clearly delineated by intense emissions of H and H 2 bands on both dayside and nightside of the planet. Emission from He is also present in the auroral regions. At Jupiter, the atmosphere was also probed by means of solar and stellar occultation experiments. The solar occultation has revealed the distribution of H 2 and H in the upper atmosphere, while the stellar occultation has probed the structure of the upper mesosphere and lower thermosphere. Current analysis indicates an eddy diffusion coefficient ∼10 6 cm² s −1 with a mesospheric temperature ∼200 K. The solar occultation analysis suggests an exospheric temperature of 1450±300 K. The thermospheric lapse rate appears to be ∼1 K/km. The Lyman α observations of the disc have revealed a longitudinal asymmetry in H which may reflect longitudinal asymmetries in Jupiter's magnetosphere. Strong EUV emission from a plasma torus at the orbit of Io has been observed in transitions of sulfur and oxygen ions with a possible small contribution from potassium. The effective electron temperature of the dense regions of the plasma is estimated to be 8 × 10 4 K. No localized EUV emission has been detected from Io, limiting mass loading at Io to ∼10 27 ions s −1 . The partitioning of ion sub‐species shows deviation from pure collisional equilibrium, but preliminary analysis indicates a low diffusive loss rate. The radiative cooling rate of the torus is ∼3 × 10 12 W. The appearance of the entire sky in the outer solar system has been mapped in the emission lines of He (584 Å) and H Lyα (1216 Å) arising from resonant scattering of the solar lines by neutral interstellar hydrogen and helium entering the solar system. Diffuse galactic EUV emission has been measured in a number of selected directions. Stellar photospheric emissions shortward of the Lyman limit of atomic hydrogen at 912 Å have been measured. Finally, spectral images, in several emission lines, have been obtained of the Cygnus Loop supernova remnant. Sections of this article review the progress in the study of these subjects and the relationships of the EUV results to the other Voyager experiments. We include a discussion of the characteristics of the instrument and the methods of spectral analysis to verify the integrity of the reported results.
    Type of Medium: Online Resource
    ISSN: 0148-0227
    Language: English
    Publisher: American Geophysical Union (AGU)
    Publication Date: 1981
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    BibTip Others were also interested in ...
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