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Possible Transient Luminous Events Observed in Jupiter's Upper Atmosphere
DOI: 10.1029/2020JE006659 Bibcode: 2020JGRE..12506659G

Wong, Michael H.; Gérard, Jean-Claude; Kammer, Joshua A. +10 more

Eleven transient bright flashes were detected in Jupiter's atmosphere using the ultraviolet spectrograph instrument on the Juno spacecraft. These bright flashes are only observed in a single spin of the spacecraft and their brightness decays exponentially with time, with a duration of ∼1.4 ms. The spectra are dominated by H2 Lyman band …

2020 Journal of Geophysical Research (Planets)
eHST 11
Late Amazonian Ice Survival in Kasei Valles, Mars
DOI: 10.1029/2020JE006531 Bibcode: 2020JGRE..12506531H

Hepburn, A. J.; Hubbard, B.; Ng, F. S. L. +1 more

High-obliquity excursions on Mars are hypothesized to have redistributed water from the poles to nourish mid-latitude glaciers. Evidence of this process is provided by different types of viscous flow features (ice-rich deposits buried beneath sediment mantle) located there today, including lobate debris aprons (LDAs). During high-obliquity extreme…

2020 Journal of Geophysical Research (Planets)
MEx 10
Updated Equipotential Shapes of Jupiter and Saturn Using Juno and Cassini Grand Finale Gravity Science Measurements
DOI: 10.1029/2019JE006354 Bibcode: 2020JGRE..12506354B

Helled, Ravit; Folkner, William M.; Parisi, Marzia +2 more

A commonly used shape model for the giant plants of Jupiter and Saturn is an oblate ellipsoid, a simplified model of the equipotential shape. The ellipsoidal shape models were originally derived from radio occultation data and gravity data after the Voyager flybys in 1979. Through precise Doppler tracking of NASA's Juno and Cassini spacecraft tele…

2020 Journal of Geophysical Research (Planets)
Cassini 10
Compositional Measurements of Saturn's Upper Atmosphere and Rings from Cassini INMS
DOI: 10.1029/2020JE006427 Bibcode: 2020JGRE..12506427S

Yelle, R. V.; Hörst, S. M.; Koskinen, T. T. +4 more

The Cassini spacecraft's last orbits directly sampled Saturn's thermosphere and revealed a much more chemically complex environment than previously believed. Observations from the Ion and Neutral Mass Spectrometer (INMS) aboard Cassini provided compositional measurements of this region and found an influx of material raining into Saturn's upper at…

2020 Journal of Geophysical Research (Planets)
Cassini 7
Relative Crater Scaling Between the Major Moons of Saturn: Implications for Planetocentric Cratering and the Surface Age of Titan
DOI: 10.1029/2020JE006392 Bibcode: 2020JGRE..12506392B

Bell, Samuel W.

The chronology of the moons of Saturn, especially Titan, has been limited by a lack of strong constraints on the cratering rate, low number statistics for small-N counts of large-diameter craters, and uncertainty about whether impactors are mostly heliocentric impactors orbiting the Sun or planetocentric impactors orbiting Saturn itself. Here, I p…

2020 Journal of Geophysical Research (Planets)
Cassini 7
Mars's Red (575-625 nm) Seasonal Approximate Reflectivity Averaged Over Mars Years 24-28 From Mars Orbiter Camera
DOI: 10.1029/2019JE006231 Bibcode: 2020JGRE..12506231R

Robbins, Stuart J.

The Mars Global Surveyor spacecraft successfully orbited Mars for over nine Earth years, its instruments returning a plethora of data that still today form important, key data sets in Mars research. A relatively underutilized data set was returned from the Mars Orbiter Camera (MOC), specifically the wide-angle component (MOC-WA), despite returning…

2020 Journal of Geophysical Research (Planets)
MEx 7
Anomalous Phyllosilicate-Bearing Outcrops South of Coprates Chasma: A Study of Possible Emplacement Mechanisms
DOI: 10.1029/2019JE006043 Bibcode: 2020JGRE..12506043B

Seelos, Frank P.; Murchie, Scott L.; Buczkowski, Debra L. +4 more

The formation of widespread phyllosilicate-bearing near-surface layers on Mars has often been attributed to pedogenesis, a process of weathering basaltic soils by continued exposure to meteoric water percolating down from the surface, which can result in layers of aluminum phyllosilicates forming over layers of iron-magnesium phyllosilicates. We p…

2020 Journal of Geophysical Research (Planets)
MEx 6
Diverse Polygonal Patterned Grounds in the Northern Eridania Basin, Mars: Possible Origins and Implications
DOI: 10.1029/2020JE006647 Bibcode: 2020JGRE..12506647D

Xiao, Long; Xu, Yi; Zhao, Jiannan +4 more

Diverse polygonal patterned grounds are found to occur in the Eridania basin system (a set of connecting irregular-shaped depressions interpreted as a paleolake basin system) located in the martian highland region between Terra Cimmeria and Sirenum. We here use multiple sets of imagery to document diverse polygonal patterned grounds in the fluvio-…

2020 Journal of Geophysical Research (Planets)
MEx 6
Tectono-Magmatic, Sedimentary, and Hydrothermal History of Arsinoes and Pyrrhae Chaos, Mars
DOI: 10.1029/2019JE006341 Bibcode: 2020JGRE..12506341L

Altieri, Francesca; Rossi, Angelo Pio; Carli, Cristian +1 more

Arsinoes and Pyrrhae Chaos are two adjacent chaotic terrains located east of Valles Marineris and west of Arabia Terra, on Mars. In this work, we produced a morpho-stratigraphic map of the area, characterized by a volcanic bedrock disrupted into polygonal mesas and knobs (Chaotic Terrain Unit) and two nondisrupted units. The latter present a spect…

2020 Journal of Geophysical Research (Planets)
MEx 5
Spatial and Temporal Variability of the 365-nm Albedo of Venus Observed by the Camera on Board Venus Express
DOI: 10.1029/2019JE006271 Bibcode: 2020JGRE..12506271L

Schröder, S. E.; Kouyama, T.; Imamura, T. +4 more

We mapped the distribution of the 365-nm albedo of the Venus atmosphere over the years 2006-2014, using images acquired by the Venus Monitoring Camera (VMC) on board Venus Express. We selected all images with a global view of Venus to investigate how the albedo depends on longitude. Bertaux et al. (2016,

VenusExpress 4