Featured
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Editorial |
The familiarity of icy worlds
The geological similarities between icy and rocky worlds invite comparison and cross-fertilization of knowledge.
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News & Views |
To sink or swim in Titan’s lakes
Flotation of aerosols as a film on the hydrocarbon lakes of Saturn’s moon Titan may explain the lakes’ stillness, and could influence the atmospheric hydrocarbon cycle.
- Isabelle Couturier-Tamburelli
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Article |
The floatability of aerosols and wave damping on Titan’s seas
Organic aerosols that sediment from Titan’s atmosphere may float, form a film and damp waves on Titan’s seas, according to computations. This damping effect could explain the observed smoothness of Titan’s seas.
- Daniel Cordier
- & Nathalie Carrasco
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Article |
Cyclonic circulation of Saturn’s atmosphere due to tilted convection
Saturn’s cyclonic atmospheric circulation may be explained by the dynamics of small-scale convection, suggest laboratory analogue experiments.
- Y. D. Afanasyev
- & Y. Zhang
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Commentary |
Cassini's Grand Finale
After more than a decade exploring Saturn and its moons, the Cassini mission is in its closing act. Cassini's last year is an encore performance stuffed with science, including a final plunge into Saturn's atmosphere.
- Scott G. Edgington
- & Linda J. Spilker
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Letter |
Simulation of deep-seated zonal jets and shallow vortices in gas giant atmospheres
Jupiter’s banded cloud layer contains enigmatic jets and vortices. Numerical simulations show that both features originate at depth in giant planet atmospheres, with vortices developing in areas of upwelling to shallow layers.
- Moritz Heimpel
- , Thomas Gastine
- & Johannes Wicht
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News & Views |
Shepherds of Saturn's ring
Saturn's F ring is chaperoned on both sides by the tiny moons Prometheus and Pandora. Numerical simulations show that this celestial ballet can result from the collision of two aggregates that evolved out of Saturn's main rings.
- Aurélien Crida
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Letter |
Saturn’s F ring and shepherd satellites a natural outcome of satellite system formation
Lying beyond Saturn’s main rings, the F ring is shepherded by two small satellites. Simulations suggest that this enigmatic configuration can result from the partial disruption of satellites in collisions at the edge of the main ring system.
- Ryuki Hyodo
- & Keiji Ohtsuki
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News & Views |
Stirring up Saturn's poles
Saturn's poles exhibit giant swirling cyclones, whereas Jupiter's poles may not. Simulations of giant planet atmospheres suggest that just the right balance of convective storm energy and poleward drift of cyclones may explain Saturn's vortices.
- Leigh N. Fletcher
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Letter |
Polar vortex formation in giant-planet atmospheres due to moist convection
Strong vortices have been observed at Saturn’s poles. Simulations suggest that tropospheric polar flows on giant planets are driven by moist convection, and that, while vortices can develop on Saturn, similar cyclones are not expected on Jupiter.
- Morgan E O’Neill
- , Kerry A. Emanuel
- & Glenn R. Flierl
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Editorial |
Planetary rite of spring
Research on the Solar System's planets has moved beyond fly-by science. Long-term observations of planetary bodies can yield insights as the days, seasons and years pass.
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Article |
Moist convection in hydrogen atmospheres and the frequency of Saturn’s giant storms
Over the past 140 years, planet-encircling storms have occurred on Saturn about every 30 years. A sufficiently wet troposphere can explain the suppression of moist convection and storm recurrence interval on Saturn.
- Cheng Li
- & Andrew P. Ingersoll
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Letter |
Common 0.1 bar tropopause in thick atmospheres set by pressure-dependent infrared transparency
In many planetary atmospheres, including that of Earth, the base of the stratosphere—the tropopause—occurs at an atmospheric pressure of 0.1 bar. A physically based model demonstrates that the pressure-dependence of transparency to infrared radiation leads to a common tropopause pressure that is probably applicable to many planetary bodies with thick atmospheres.
- T. D. Robinson
- & D. C. Catling
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Letter |
Atmospheric dynamics of Saturn’s 2010 giant storm
Great White Spot—a rare planet-encircling storm—raged on Saturn in 2010–2011. Analyses of high-resolution spacecraft imagery and numerical modelling reveal a dynamic storm head powered by sustained convection in the zonal flow of Saturn’s atmosphere.
- E. García-Melendo
- , R. Hueso
- & J. F. Sanz-Requena
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Letter |
Layered convection as the origin of Saturn’s luminosity anomaly
Saturn is brighter than expected for a gas giant of its age. Calculations of Saturn’s thermal evolution show that the presence of layered convection in Saturn’s interior—much like that observed in the Earth’s oceans—would have slowed the planet’s cooling and may explain Saturn’s anomalous luminosity.
- Jérémy Leconte
- & Gilles Chabrier
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Letter |
Equatorial winds on Saturn and the stratospheric oscillation
The stability over time of the zonal jets on the giant planets has been debated. An analysis of observations from the Cassini spacecraft reveals an acceleration of wind velocities in Saturn’s high-altitude equatorial jet between 2004 and 2009, by 20 m s−1 at tropopause level and by 60 m s−1 in the stratosphere.
- Liming Li
- , Xun Jiang
- & Kevin H. Baines