• Title of article

    Small-scale temperature fluctuations seen by the VeRa Radio Science Experiment on Venus Express

  • Author/Authors

    Tellmann، نويسنده , , S. and Hنusler، نويسنده , , B. and Hinson، نويسنده , , D.P. and Tyler، نويسنده , , G.L. and Andert، نويسنده , , T.P. and Bird، نويسنده , , M.K. and Imamura، نويسنده , , T. and Pنtzold، نويسنده , , M. and Remus، نويسنده , , S.، نويسنده ,

  • Issue Information
    روزنامه با شماره پیاپی سال 2012
  • Pages
    10
  • From page
    471
  • To page
    480
  • Abstract
    The Venus Express Radio Science Experiment VeRa retrieves atmospheric profiles in the mesosphere and troposphere of Venus in the approximate altitude range of 40–90 km. A data set of more than 500 profiles was retrieved between the orbit insertion of Venus Express in 2006 and the end of occultation season No. 11 in July 2011. The atmospheric profiles cover a wide range of latitudes and local times, enabling us to study the dependence of vertical small-scale temperature perturbations on local time and latitude. ature fluctuations with vertical wavelengths of 4 km or less are extracted from the measured temperature profiles in order to study small-scale gravity waves. Significant wave amplitudes are found in the stable atmosphere above the tropopause at roughly 60 km as compared with the only shallow temperature perturbations in the nearly adiabatic region of the adjacent middle cloud layer, below. y wave activity shows a strong latitudinal dependence with the smallest wave amplitudes located in the low-latitude range, and an increase of wave activity with increasing latitude in both hemispheres; the greatest wave activity is found in the high-northern latitude range in the vicinity of Ishtar Terra, the highest topographical feature on Venus. d evidence for a local time dependence of gravity wave activity in the low latitude range within ±30° of the equator. Gravity wave amplitudes are at their maximum beginning at noon and continuing into the early afternoon, indicating that convection in the lower atmosphere is a possible wave source. mparison of the measured vertical wave structures with standard linear-wave theory allows us to derive rough estimates of the wave intrinsic frequency and horizontal wavelengths, assuming that the observed wave structures are the result of pure internal gravity waves. Horizontal wavelengths of the waves at 65 km altitude are on the order of ≈300–450 km with horizontal phase speeds of roughly 5–10 m/s.
  • Keywords
    Atmospheres , Dynamics , occultations , Radio observations , Venus
  • Journal title
    Icarus
  • Serial Year
    2012
  • Journal title
    Icarus
  • Record number

    2379355