From a misinterpretation of Mariner 10 pictures, Chamberlain (1974) constructed a model in which he used horizontal variations in the Venus atmosphere to explain the phase-variation of CO2 absorption at small phase angles. Published observations of spatial variations in CO2 absorption on Venus show that they are too small to explain the phase effect. The question of uniqueness that is, if more than one model can explain the phase-effect observations is discussed. Before this question can be answered, a realistic model that does account for the data must be constructed. No such calculations exist
The exploration of Venus continues to be a top priority of planetary science. The Planetary Decadal ...
Similarities in the size and mean density of Earth and Venus encourage the use of Earth-analogue mod...
AbstractWe have analyzed the long-term regional and global variation of emitted radiance in 1.74 µ m...
The evolution of our solar system remains one of the most fascinating questions since ancient astron...
The physical and chemical properties of the clouds of Venus are reviewed, with special emphasis on d...
The spectral and polarization data for Venus are consistent with micron-sized, aerosol cloud particl...
Observations of the short period variations in ultraviolet polarization and carbon dioxide line inte...
International audienceBased on the HSTobserved LST and latitude albedo variations we conclu...
Comments on ice particles as major scatterers of infrared radiation from Venus atmospher
Venus formed in the same part of our solar system as Earth, apparently from similar materials. Altho...
The two defining characteristics of the planet Venus are its atmospheric super-rotation and the plan...
International audienceThe lower atmosphere of Venus below the clouds is a transitional region betwee...
The principal theme of this thesis is to see the planetary processes underlying observable variation...
International audienceVenus' cloud top region exhibits a higher level of variability both in space a...
Water is a key constituent of every planetary environment, and on Venus its abundance, distribution ...
The exploration of Venus continues to be a top priority of planetary science. The Planetary Decadal ...
Similarities in the size and mean density of Earth and Venus encourage the use of Earth-analogue mod...
AbstractWe have analyzed the long-term regional and global variation of emitted radiance in 1.74 µ m...
The evolution of our solar system remains one of the most fascinating questions since ancient astron...
The physical and chemical properties of the clouds of Venus are reviewed, with special emphasis on d...
The spectral and polarization data for Venus are consistent with micron-sized, aerosol cloud particl...
Observations of the short period variations in ultraviolet polarization and carbon dioxide line inte...
International audienceBased on the HSTobserved LST and latitude albedo variations we conclu...
Comments on ice particles as major scatterers of infrared radiation from Venus atmospher
Venus formed in the same part of our solar system as Earth, apparently from similar materials. Altho...
The two defining characteristics of the planet Venus are its atmospheric super-rotation and the plan...
International audienceThe lower atmosphere of Venus below the clouds is a transitional region betwee...
The principal theme of this thesis is to see the planetary processes underlying observable variation...
International audienceVenus' cloud top region exhibits a higher level of variability both in space a...
Water is a key constituent of every planetary environment, and on Venus its abundance, distribution ...
The exploration of Venus continues to be a top priority of planetary science. The Planetary Decadal ...
Similarities in the size and mean density of Earth and Venus encourage the use of Earth-analogue mod...
AbstractWe have analyzed the long-term regional and global variation of emitted radiance in 1.74 µ m...