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HST/WFC3 observations of Uranus' 2014 storm clouds and comparison with VLT/SINFONI and IRTF/Spex observations
DOI: 10.1016/j.icarus.2017.01.031 Bibcode: 2017Icar..288...99I

Wong, Michael H.; Irwin, Patrick G. J.; Orton, G. S. +2 more

In November 2014 Uranus was observed with the Wide Field Camera 3 (WFC3) instrument of the Hubble Space Telescope as part of the Hubble 2020: Outer Planet Atmospheres Legacy program, OPAL. OPAL annually maps Jupiter, Uranus and Neptune (and will also map Saturn from 2018) in several visible/near-infrared wavelength filters. The Uranus 2014 OPAL ob…

2017 Icarus
eHST 25
Similarity of the Jovian satellite footprints: Spots multiplicity and dynamics
DOI: 10.1016/j.icarus.2017.01.009 Bibcode: 2017Icar..292..208B

Saur, J.; Badman, S. V.; Bonfond, B. +3 more

In the magnetospheres of Jupiter and Saturn, the intense interaction of the satellites Io, Europa, Ganymede and Enceladus with their surrounding plasma environment leaves a signature in the aurora of the planet. Called satellite footprints, these auroral features appear either as a single spot (Europa and Enceladus) or as multiple spots (Io and Ga…

2017 Icarus
eHST 25
Overview of useful spectral regions for Venus: An update to encourage observations complementary to the Akatsuki mission
DOI: 10.1016/j.icarus.2017.01.027 Bibcode: 2017Icar..288..235P

Sánchez-Lavega, A.; Widemann, T.; Imamura, T. +5 more

New tables to observe the planet Venus are presented with detailed information about the main spectral regions from 100 nm to 1 mm. The information hereby is updated thanks to the Venus Express legacy and recent ground-based observations, and we hope it can constitute a helpful tool for professional and amateur observers willing to support and coo…

2017 Icarus
VenusExpress 24
The Mars diffuse aurora: A model of ultraviolet and visible emissions
DOI: 10.1016/j.icarus.2017.01.037 Bibcode: 2017Icar..288..284G

Gérard, J. -C.; Soret, L.; Shematovich, V. I. +2 more

A new type of Martian aurora, characterized by an extended spatial distribution, an altitude lower than the discrete aurora and electron precipitation up to 200 keV has been observed following solar activity on several occasions from the MAVEN spacecraft. We describe the results of Monte Carlo simulations of the production of several ultraviolet a…

2017 Icarus
MEx 24
Statistical study of Saturn's auroral electron properties with Cassini/UVIS FUV spectral images
DOI: 10.1016/j.icarus.2016.11.017 Bibcode: 2017Icar..284..264G

Lamy, L.; Grodent, D.; Radioti, A. +3 more

About 2000 FUV spectra of different regions of Saturn's aurora, obtained with Cassini/UVIS from December 2007 to October 2014 have been examined. Two methods have been employed to determine the mean energy <;E> of the precipitating electrons. The first is based on the absorption of the auroral emission by hydrocarbons and the second uses the…

2017 Icarus
Cassini 23
Cassini ISS observation of Saturn's north polar vortex and comparison to the south polar vortex
DOI: 10.1016/j.icarus.2016.12.011 Bibcode: 2017Icar..285...68S

Dyudina, Ulyana A.; Ingersoll, Andrew P.; Ewald, Shawn P. +2 more

We present analyses of Saturn's north pole using high-resolution images captured in late 2012 by the Cassini spacecraft's Imaging Science Subsystem (ISS) camera. The images reveal the presence of an intense cyclonic vortex centered at the north pole. In the red and green visible continuum wavelengths, the north polar region exhibits a cyclonically…

2017 Icarus
Cassini 22
Neptune long-lived atmospheric features in 2013-2015 from small (28-cm) to large (10-m) telescopes
DOI: 10.1016/j.icarus.2017.06.009 Bibcode: 2017Icar..295...89H

Hueso, R.; Sánchez-Lavega, A.; Rojas, J. F. +32 more

Since 2013, observations of Neptune with small telescopes (28-50 cm) have resulted in several detections of long-lived bright atmospheric features that have also been observed by large telescopes such as Keck II or Hubble. The combination of both types of images allows the study of the long-term evolution of major cloud systems in the planet. In 2…

2017 Icarus
eHST 22
The effect of asymmetric surface topography on dust dynamics on airless bodies
DOI: 10.1016/j.icarus.2017.03.019 Bibcode: 2017Icar..291...65P

Horányi, M.; Piquette, M.

Without a significant atmosphere or global magnetic field, the lunar surface is exposed to micrometeoroid bombardment, ultraviolet (UV) radiation, and the solar wind. Micrometeoroid bombardment grinds the surface into a regolith comprised of dust grains ranging in size from 10 nm to 1 mm (Grün et al., 2011). Incident UV radiation and solar wind el…

2017 Icarus
Rosetta 22
Brittle ice shell thickness of Enceladus from fracture distribution analysis
DOI: 10.1016/j.icarus.2017.07.009 Bibcode: 2017Icar..297..252L

Cremonese, G.; Massironi, M.; Lucchetti, A. +2 more

We determine the depth of fracture penetration in multiple regions of Enceladus by performing self-similar clustering and length distribution analysis of fractures. The statistical characterization of fault-population attribute, such as length and clustering, provide a productive avenue for exploring deformation rate, stress transmission mode, rhe…

2017 Icarus
Cassini 21
Geology and mineralogy of the Auki Crater, Tyrrhena Terra, Mars: A possible post impact-induced hydrothermal system
DOI: 10.1016/j.icarus.2016.09.001 Bibcode: 2017Icar..281..228C

Bellucci, G.; Carrozzo, F. G.; Altieri, F. +2 more

A variety of hydrothermal environments have been documented in terrestrial impact structures. Due to both past water interactions and meteoritic bombardment on the surface of Mars, several authors have predicted various scenarios that include the formation of hydrothermal systems. Geological and mineralogical evidence of past hydrothermal activity…

2017 Icarus
MEx 21