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Thermal structure in the Venus middle cloud layerThermal structure measurements obtained by the two Vega balloons show the Venus atmosphere in the middle cloud layer to be near-adiabatic, on the whole; but discrete air masses are present that differ slightly from one another in potential temperature and entropy. The Vega 1 temperatures are 6.5 K warmer than measured by Vega 2 at given pressures. Measurements taken by the Vega 2 lander on descent through these levels agree with the Vega 2 balloon data.
Document ID
19870032283
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Linkin, V. M.
(Academy of Sciences (USSR) Moscow, Ussr)
Lipatov, A. N.
(Academy of Sciences (USSR) Moscow, Ussr)
Shurupov, A. A.
(Academy of Sciences (USSR) Moscow, Ussr)
Ignatova, S. P.
(Academy of Sciences (USSR) Moscow, Ussr)
Frank, G. A.
(AN SSSR, Institut Kosmicheskikh Issledovanii, Moscow, USSR Moscow, Ussr)
Seiff, A.
(Academy of Sciences (USSR) Moscow, Ussr)
Ragent, B.
(Academy of Sciences (USSR) Moscow, Ussr)
Young, R. E.
(NASA Ames Research Center, Moffett Field, CA)
Elson, L. S.
(Academy of Sciences (USSR))
Preston, R. A.
(California Institute of Technology, Jet Propulsion Laboratory, Pasadena)
Date Acquired
August 13, 2013
Publication Date
February 1, 1986
Publication Information
Publication: Soviet Astronomy Letters
Volume: 12
ISSN: 0360-0327
Subject Category
Lunar And Planetary Exploration
Accession Number
87A19557
Distribution Limits
Public
Copyright
Other

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