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1939
In this paper the two model of Jupiter’s atmosphere, vi., adiabatic and isothermal, have been considered. The variability of the period of rotation of the atmosphere depending on the latitude and the variation of gravity have both been taken into account.The datum level of Jupiter is the effective radiating and absorbing layer probably a cloud layer at
Banerji, A C, Nizamuddin
openaire +1 more source
In this paper the two model of Jupiter’s atmosphere, vi., adiabatic and isothermal, have been considered. The variability of the period of rotation of the atmosphere depending on the latitude and the variation of gravity have both been taken into account.The datum level of Jupiter is the effective radiating and absorbing layer probably a cloud layer at
Banerji, A C, Nizamuddin
openaire +1 more source
WHOLE ATMOSPHERE MODELING: CONNECTING TERRESTRIAL AND SPACE WEATHER
Reviews of Geophysics, 2011R A Akmaev
exaly

