Search Publications

Constraining the thermal properties of planetary surfaces using machine learning: Application to airless bodies
DOI: 10.1016/j.icarus.2019.01.017 Bibcode: 2019Icar..325...16C

Furfaro, Roberto; Cambioni, Saverio; Delbo, Marco +2 more

We present a new method for the determination of the surface properties of airless bodies from measurements of the emitted infrared flux. Our approach uses machine learning techniques to train, validate, and test a neural network representation of the thermophysical behavior of the atmosphereless body given shape model, illumination and observatio…

2019 Icarus
AKARI 15
The Martian daytime convective boundary layer: Results from radio occultation measurements and a mesoscale model
DOI: 10.1016/j.icarus.2019.02.028 Bibcode: 2019Icar..326..105H

Pätzold, M.; Hinson, D. P.; Häusler, B. +4 more

We investigate the behavior of the Martian daytime convective boundary layer (CBL) through a combination of data analysis and modeling. This study relies on two subsets of Mars Express radio occultation (RO) measurements that sounded the atmosphere in northern spring of successive Mars years. Only the first year of observations has been examined p…

2019 Icarus
MEx 15
Araneiform terrain formation in Angustus Labyrinthus, Mars
DOI: 10.1016/j.icarus.2018.07.026 Bibcode: 2019Icar..317..479H

Jaumann, R.; Hao, J.; Michael, G. G. +1 more

The south polar area of Mars exhibits an abundance of distinctive and exotic landforms, most of which occur within the region covered by the seasonal CO2 cap. Araneiform terrain (also referred to as terrain covered by "spiders") is one of these unusual geomorphic features, resulting from CO2 sublimation driven seasonal erosio…

2019 Icarus
MEx 15
Fine-scale structure in cometary dust tails I: Analysis of striae in Comet C/2006 P1 (McNaught) through temporal mapping
DOI: 10.1016/j.icarus.2018.09.013 Bibcode: 2019Icar..319..540P

Morgan, Huw; Jones, Geraint H.; Battams, Karl +5 more

Striated features, or striae, form in cometary dust tails due to an as-yet unconstrained process or processes. For the first time we directly display the formation of striae, at C/2006 P1 McNaught, using data from the SOHO LASCO C3 coronagraph. The nature of this formation suggests both fragmentation and shadowing effects are important in the form…

2019 Icarus
SOHO 14
A stellar occultation by Vanth, a satellite of (90482) Orcus
DOI: 10.1016/j.icarus.2018.10.016 Bibcode: 2019Icar..319..657S

Bosh, A. S.; Lister, T. A.; Schindler, K. +5 more

A stellar occultation by the large trans-Neptunian object (90482) Orcus was predicted to occur on 2017 March 07. Observations were made at five sites in North and South America: the 0.6-m Astronomical Telescope of the University of Stuttgart (ATUS) at Sierra Remote Observatories, California; Las Cumbres Observatory's 1-m telescope at McDonald Obse…

2019 Icarus
Gaia 14
Interior properties of the inner Saturnian moons from space astrometry data
DOI: 10.1016/j.icarus.2019.01.026 Bibcode: 2019Icar..326...48L

Lainey, V.; Noyelles, B.; Rambaux, N. +3 more

During the thirteen years in orbit around Saturn before its final plunge, the Cassini spacecraft provided more than ten thousand astrometric measurements. Such large amounts of accurate data enable the search for extremely faint signals in the orbitalmotion of the saturnian moons. Among these, the detection of the dynamical feedback of the rotatio…

2019 Icarus
Cassini eHST 14
Studies of irregular satellites: I. Lightcurves and rotation periods of 25 Saturnian moons from Cassini observations
DOI: 10.1016/j.icarus.2018.12.040 Bibcode: 2019Icar..322...80D

Mottola, Stefano; Denk, Tilmann

Disk-integrated time-resolved photometric observations have been performed for 25 irregular moons of Saturn with the ISS camera of the Cassini spacecraft in a wide range of solar phase angles. From the derived lightcurves, synodic rotation periods were determined, ranging from 5.5 h to 76 h; the fastest observed spin rate is much slower than the d…

2019 Icarus
Cassini 14
An equatorial thermal wind equation: Applications to Jupiter
DOI: 10.1016/j.icarus.2018.09.037 Bibcode: 2019Icar..324..198M

Wong, Michael H.; Tollefson, Joshua; Marcus, Philip S. +1 more

To relate the vertical wind shear to horizontal temperature gradients at and near the equator, we derive an "Equatorial Thermal Wind Equation" (EQTWE) using a minimum set of assumptions that are easily satisfied for the atmospheres of all the giant planets and Earth. Similar to the textbook Thermal Wind Equation (TWE), the EQTWE requires a small R…

2019 Icarus
eHST 13
Ultraviolet observation of Enceladus' plume in transit across Saturn, compared to Europa
DOI: 10.1016/j.icarus.2019.04.031 Bibcode: 2019Icar..330..256H

Hansen, C. J.; Hendrix, A. R.; Esposito, L. W.

Saturn's moon Enceladus is known to have a water vapor plume erupting from fissures across its south polar region. The plume was detectable in an observation of Enceladus transiting Saturn by Cassini's Ultraviolet Imaging Spectrograph (UVIS), but only at 1216 Å (Lyman alpha). Jupiter's moon Europa also may have multiple water vapor plumes, detecte…

2019 Icarus
Cassini 13
First measurements of Jupiter's zonal winds with visible imaging spectroscopy
DOI: 10.1016/j.icarus.2018.10.019 Bibcode: 2019Icar..319..795G

Sato, Bun'ei; Rivet, Jean-Pierre; Guillot, Tristan +12 more

We present the first measurements of Jupiter's wind profile ever obtained with Doppler velocity measurements in the visible. Hitherto, knowledge about atmospheric dynamics has been obtained with cloud-tracking techniques, which consist of tracking visible features from images taken at different dates. However, cloud tracking indicates the motion o…

2019 Icarus
eHST 13