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VIRTIS emissivity of Alpha Regio, Venus, with implications for tessera composition
DOI: 10.1016/j.icarus.2015.04.008 Bibcode: 2015Icar..254..350G

Gilmore, Martha S.; Helbert, Jörn; Mueller, Nils

The composition of Venus tessera terrain is unknown. The Visible and Infrared Thermal Imaging Spectrometer (VIRTIS) aboard Venus Express (VEx) collects data that yields the surface emissivity at ∼1 µm, which contains information convolving a number of surface properties, including composition. We examine the variation of emissivity in the vi…

2015 Icarus
VenusExpress 63
Thermal evolution of Venus with argon degassing
DOI: 10.1016/j.icarus.2015.07.009 Bibcode: 2015Icar..260..128O

O'Rourke, Joseph G.; Korenaga, Jun

Decades-old measurements of atmospheric and elemental surface composition constrain the history of Venus. In this study, we search for a model featuring continuous evolution in the stagnant-lid regime that predicts the present-day atmospheric mass of radiogenic argon and satisfies the other available constraints. For comparison, we also consider t…

2015 Icarus
VenusExpress 52
Lithospheric structure of Venus from gravity and topography
DOI: 10.1016/j.icarus.2015.07.020 Bibcode: 2015Icar..260..215J

Ruiz, Javier; Jiménez-Díaz, Alberto; Kirby, Jon F. +3 more

There are many fundamental and unanswered questions on the structure and evolution of the venusian lithosphere, which are key issues for understanding Venus in the context of the origin and evolution of the terrestrial planets. Here we investigate the lithospheric structure of Venus by calculating its crustal and effective elastic thicknesses (T

2015 Icarus
VenusExpress 49
Vertical profiles of H2O, H2SO4, and sulfuric acid concentration at 45-75 km on Venus
DOI: 10.1016/j.icarus.2015.01.024 Bibcode: 2015Icar..252..327K

Krasnopolsky, Vladimir A.

A method developed by Krasnopolsky and Pollack (Krasnopolsky, V.A., Pollack, J.B. [1994]. Icarus 109, 58-78) to model vertical profiles of H2O and H2SO4 vapors and sulfuric acid concentration in the Venus cloud layer has been updated with improved thermodynamic parameters for H2O and H2SO

2015 Icarus
VenusExpress 45
Constraints on a potential aerial biosphere on Venus: I. Cosmic rays
DOI: 10.1016/j.icarus.2015.05.006 Bibcode: 2015Icar..257..396D

Coates, Andrew J.; Jones, Geraint H.; Patel, Manish R. +3 more

While the present-day surface of Venus is certainly incompatible with terrestrial biology, the planet may have possessed oceans in the past and provided conditions suitable for the origin of life. Venusian life may persist today high in the atmosphere where the temperature and pH regime is tolerable to terrestrial extremophile microbes: an aerial …

2015 Icarus
VenusExpress 39
Coordinated Hubble Space Telescope and Venus Express Observations of Venus' upper cloud deck
DOI: 10.1016/j.icarus.2015.05.027 Bibcode: 2015Icar..258..309J

Bertaux, Jean-Loup; Marcq, Emmanuel; Wilson, Colin +10 more

Hubble Space Telescope Imaging Spectrograph (HST/STIS) UV observations of Venus' upper cloud tops were obtained between 20N and 40S latitude on December 28, 2010; January 22, 2011 and January 27, 2011 in coordination with the Venus Express (VEx) mission. The high spectral (0.27 nm) and spatial (40-60 km/pixel) resolution HST/STIS data provide the …

2015 Icarus
VenusExpress eHST 38
Long-term variations of the UV contrast on Venus observed by the Venus Monitoring Camera on board Venus Express
DOI: 10.1016/j.icarus.2015.02.015 Bibcode: 2015Icar..253....1L

Schröder, S. E.; Imamura, T.; Marcq, E. +1 more

We analyze the Venus ultraviolet (UV) reflectivity as observed by the Venus Monitoring Camera on board Venus Express over 2000 orbits in the years 2006-2011. We compare several laws for the photometric correction of global images of Venus, and find that the combined law of Lambert and Lommel-Seeliger is most suitable for our study. Our analysis of…

2015 Icarus
VenusExpress 36
Ionization of the venusian atmosphere from solar and galactic cosmic rays
DOI: 10.1016/j.icarus.2014.09.032 Bibcode: 2015Icar..245...80N

Coates, A. J.; Jones, G. H.; Desorgher, L. +2 more

The atmospheres of the terrestrial planets are exposed to solar and galactic cosmic rays, the most energetic of which are capable of affecting deep atmospheric layers through extensive nuclear and electromagnetic particle cascades. In the venusian atmosphere, cosmic rays are expected to be the dominant ionization source below ∼100 km altitude. Whi…

2015 Icarus
VenusExpress 35
Vertical propagation of planetary-scale waves in variable background winds in the upper cloud region of Venus
DOI: 10.1016/j.icarus.2014.07.011 Bibcode: 2015Icar..248..560K

Futaana, Yoshifumi; Imamura, Takeshi; Kouyama, Toru +2 more

Recently it was found that the low-latitude zonal wind and the amplitudes of Kelvin and Rossby waves at the cloud top of Venus show long-term variations in a synchronized manner. For the purpose of explaining this synchronization, we investigated the influence of the background zonal wind profile on the upward propagation of Kelvin and Rossby wave…

2015 Icarus
VenusExpress 33
Carbon monoxide and temperature in the upper atmosphere of Venus from VIRTIS/Venus Express non-LTE limb measurements
DOI: 10.1016/j.icarus.2014.10.047 Bibcode: 2015Icar..248..478G

López-Valverde, M. A.; Gilli, G.; Drossart, P. +4 more

The upper mesosphere and the lower thermosphere of Venus (from 90 to 150 km altitude) seems to play a transition region in photochemistry, dynamics and radiation, but is still very poorly constrained observationally. Since 2006 VIRTIS on board Venus Express has been obtaining limb observations of CO fluorescent infrared emissions in a systematic m…

2015 Icarus
VenusExpress 25