Search Publications

Modelled isotopic fractionation and transient diffusive release of methane from potential subsurface sources on Mars
DOI: 10.1016/j.icarus.2016.08.023 Bibcode: 2017Icar..281..240S

Stevens, Adam H.; Lewis, Stephen R.; Patel, Manish R.

We calculate transport timescales of martian methane and investigate the effect of potential release mechanisms into the atmosphere using a numerical model that includes both Fickian and Knudsen diffusion. The incorporation of Knudsen diffusion, which improves on a Fickian description of transport given the low permeability of the martian regolith…

2017 Icarus
ExoMars-16 9
The photochemical fractionation of oxygen isotopologues in Titan's atmosphere
DOI: 10.1016/j.icarus.2017.02.032 Bibcode: 2017Icar..291...17L

Dobrijevic, M.; Loison, J. C.; Hickson, K. M. +1 more

The origin of CO and the external source of H2O in the atmosphere of Titan is still a matter of debate. We investigated the chemical fractionation of oxygen isotopologues in order to give new constraints on the origin of oxygen species. We created a new chemical scheme and we developed a 1-D time-dependent photochemical model to compute…

2017 Icarus
Cassini 9
The effect of like-charge attraction on aerosol growth in the atmosphere of Titan
DOI: 10.1016/j.icarus.2016.12.013 Bibcode: 2017Icar..291..245L

Lindgren, Eric B.; Stamm, Benjamin; Chan, Ho-Kei +3 more

The formation of aerosols in the atmosphere of Titan is based extensively on ion-neutral chemistry and physical condensation processes. Herein it is shown that the formation of aerosols may also occur through an alternative pathway that involves the physical aggregation of negatively charged particles, which are known to be abundant in the satelli…

2017 Icarus
Cassini 9
Dawn-dusk difference of periodic oxygen EUV dayglow variations at Venus observed by Hisaki
DOI: 10.1016/j.icarus.2016.12.027 Bibcode: 2017Icar..292..102M

Leblanc, François; Tsuchiya, Fuminori; Seki, Kanako +8 more

We report a dawn-dusk difference of periodic variations of oxygen EUV dayglow (OII 83.4 nm, OI 130.4 nm and OI 135.6 nm) in the upper atmosphere of Venus observed by the Hisaki spacecraft in 2015. Observations show that the periodic dayglow variations are mainly controlled by the solar EUV flux. Additionally, we observed characteristic ∼1 day and …

2017 Icarus
VenusExpress 9
Radiative energy balance of Venus: An approach to parameterize thermal cooling and solar heating rates
DOI: 10.1016/j.icarus.2016.11.025 Bibcode: 2017Icar..284..216H

Kappel, D.; Arnold, G.; Haus, R.

Thermal cooling rates QC and solar heating rates QH in the atmosphere of Venus at altitudes between 0 and 100 km are investigated using the radiative transfer and radiative balance simulation techniques described by Haus et al. (2015b, 2016). QC strongly responds to temperature profile and cloud parameter changes, …

2017 Icarus
VenusExpress 9
Diurnal observations of HCl altitude variation in the 70-100 km mesosphere of Venus
DOI: 10.1016/j.icarus.2017.02.017 Bibcode: 2017Icar..290..156S

Todd Clancy, R.; Sandor, Brad J.

First submm spectroscopic observations of the 625.9 GHz H35Cl absorption lines of the Venus dayside atmosphere were obtained with the James Clerk Maxwell Telescope (JCMT) on March 2, 2013. These data, which support retrieval of HCl altitude distributions in the Venus mesosphere (70-100 km), are presented here and compared with previousl…

2017 Icarus
VenusExpress 9
Clastic patterned ground in Lomonosov crater, Mars: examining fracture controlled formation mechanisms
DOI: 10.1016/j.icarus.2017.06.008 Bibcode: 2017Icar..295..125B

Balme, Matthew R.; Patel, Manish R.; Hagermann, Axel +1 more

The area surrounding Lomonosov crater on Mars has a high density of seemingly organised boulder patterns. These form seemingly sorted polygons and stripes within kilometre scale blockfields, patches of boulder strewn ground which are common across the Martian high latitudes. Several hypotheses have been suggested to explain the formation of clasti…

2017 Icarus
MEx 9
The reflectivity of Mars at 1064 nm: Derivation from Mars Orbiter Laser Altimeter data and application to climatology and meteorology
DOI: 10.1016/j.icarus.2017.01.032 Bibcode: 2017Icar..289....1H

Heavens, N. G.

The Mars Orbiter Laser Altimeter (MOLA) on board Mars Global Surveyor (MGS) made > 108 measurements of the reflectivity of Mars at 1064 nm (R1064) by both active sounding and passive radiometry. Past studies of R1064 neglected the effects of atmospheric opacity and viewing geometry on both active and passive mea…

2017 Icarus
eHST 8
Discovery of a 150 day period in the Venus condensational clouds
DOI: 10.1016/j.icarus.2016.10.005 Bibcode: 2017Icar..286..118M

Tsang, Constantine C. C.; McGouldrick, Kevin

We have analyzed the long-term regional and global variation of emitted radiance in 1.74 µ m and 2.30 µ m near infrared spectral windows in the Venus atmosphere using the medium resolution, infrared channel of the Visible and Infrared Thermal Imaging Spectrometer (VIRTIS-M-IR) on the Venus Express spacecraft. We find a periodic variati…

2017 Icarus
VenusExpress 8
Search for HBr and bromine photochemistry on Venus
DOI: 10.1016/j.icarus.2017.04.016 Bibcode: 2017Icar..293..114K

Krasnopolsky, Vladimir A.; Belyaev, Denis A.

HBr (1-0) R2 2605.8/6.2 cm-1, the strongest line of the strongest band of HBr, was observed when searching for this species on Venus. The observation was conducted using the NASA IRTF and a high-resolution long-slit spectrograph CSHELL with resolving power of 4 × 104. 101 spectra of Venus were analyzed, and the retrieved HBr …

2017 Icarus
VenusExpress 7