Search Publications

Ongoing hydrothermal activities within Enceladus
DOI: 10.1038/nature14262 Bibcode: 2015Natur.519..207H

Postberg, Frank; Altobelli, Nicolas; Sekine, Yasuhito +12 more

Detection of sodium-salt-rich ice grains emitted from the plume of the Saturnian moon Enceladus suggests that the grains formed as frozen droplets from a liquid water reservoir that is, or has been, in contact with rock. Gravitational field measurements suggest a regional south polar subsurface ocean of about 10 kilometres thickness located beneat…

2015 Nature
Cassini 338
The pH of Enceladus' ocean
DOI: 10.1016/j.gca.2015.04.017 Bibcode: 2015GeCoA.162..202G

Glein, Christopher R.; Waite, J. Hunter; Baross, John A.

Saturn's moon, Enceladus, is a geologically active waterworld. The prevailing paradigm is that there is a subsurface ocean that erupts to the surface, which leads to the formation of a plume of vapor and ice above the south polar region. The chemistry of the ocean is just beginning to be understood, but is of profound geochemical and astrobiologic…

2015 Geochimica et Cosmochimica Acta
Cassini 170
GCM simulations of Titan's middle and lower atmosphere and comparison to observations
DOI: 10.1016/j.icarus.2014.12.030 Bibcode: 2015Icar..250..516L

Lunine, Jonathan I.; Lora, Juan M.; Russell, Joellen L.

Simulation results are presented from a new general circulation model (GCM) of Titan, the Titan Atmospheric Model (TAM), which couples the Flexible Modeling System (FMS) spectral dynamical core to a suite of external/sub-grid-scale physics. These include a new non-gray radiative transfer module that takes advantage of recent data from Cassini-Huyg…

2015 Icarus
Cassini 107
Effect of Enceladus's rapid synchronous spin on interpretation of Cassini gravity
DOI: 10.1002/2015GL063384 Bibcode: 2015GeoRL..42.2137M

McKinnon, William B.

Enceladus's degree 2 gravity, determined by Cassini, is nominally nonhydrostatic to 3σ (J2/C22 = 3.38-3.63, as opposed to 10/3). Iess et al. (2014) interpret this in terms of a hydrostatic interior (core) and isostatic (not hydrostatic) floating ice shell. Enceladus's rapid (1.37 d) synchronous spin and tide distorts its shap…

2015 Geophysical Research Letters
Cassini 100
Seasonal variations in Titan's middle atmosphere during the northern spring derived from Cassini/CIRS observations
DOI: 10.1016/j.icarus.2014.11.019 Bibcode: 2015Icar..250...95V

Bézard, Bruno; Vinatier, Sandrine; Achterberg, Richard K. +8 more

We analyzed spectra acquired at the limb of Titan in the 2006-2013 period by the Cassini/Composite Infrared Spectrometer (CIRS) in order to monitor the seasonal evolution of the thermal, gas composition and aerosol spatial distributions. We are primarily interested here in the seasonal changes after the northern spring equinox and interpret our re…

2015 Icarus
Cassini 81
Field-aligned currents in Saturn's northern nightside magnetosphere: Evidence for interhemispheric current flow associated with planetary period oscillations
DOI: 10.1002/2015JA021454 Bibcode: 2015JGRA..120.7552H

Coates, A. J.; Dougherty, M. K.; Alexeev, I. I. +6 more

We investigate the magnetic perturbations associated with field-aligned currents observed on 34 Cassini passes over the premidnight northern auroral region during 2008. These are found to be significantly modulated not only by the northern planetary-period oscillation (PPO) system, similar to the southern currents by the southern PPO system found …

2015 Journal of Geophysical Research (Space Physics)
Cassini 65
Nature of the MHD and Kinetic Scale Turbulence in the Magnetosheath of Saturn: Cassini Observations
DOI: 10.1088/2041-8205/813/2/L29 Bibcode: 2015ApJ...813L..29H

Dougherty, M. K.; Sahraoui, F.; Masters, A. +5 more

Low-frequency turbulence in Saturn’s magnetosheath is investigated using in situ measurements of the Cassini spacecraft. Focus is put on the magnetic energy spectra computed in the frequency range of ∼[10-4, 1]Hz. A set of 42 time intervals in the magnetosheath were analyzed, and three main results that contrast with known features of s…

2015 The Astrophysical Journal
Cassini 64
Structural mapping of Enceladus and implications for formation of tectonized regions
DOI: 10.1002/2015JE004818 Bibcode: 2015JGRE..120..928C

Crow-Willard, Emma N.; Pappalardo, Robert T.

Global structural mapping of high-resolution Cassini images of Enceladus reveals a richly varied surface. Most notable are three main regions of deformation each containing multiple structural units. In addition to the well known "South Polar Terrain" (SPT), there are two other large regions of deformation that we term "Leading Hemisphere Terrain"…

2015 Journal of Geophysical Research (Planets)
Cassini 60
Curtain eruptions from Enceladus' south-polar terrain
DOI: 10.1038/nature14368 Bibcode: 2015Natur.521...57S

Spitale, Joseph N.; Hurford, Terry A.; Rhoden, Alyssa R. +2 more

Observations of the south pole of the Saturnian moon Enceladus revealed large rifts in the south-polar terrain, informally called `tiger stripes', named Alexandria, Baghdad, Cairo and Damascus Sulci. These fractures have been shown to be the sources of the observed jets of water vapour and icy particles and to exhibit higher temperatures than the …

2015 Nature
Cassini 52
Possible evidence for a methane source in Enceladus' ocean
DOI: 10.1002/2014GL063013 Bibcode: 2015GeoRL..42.1334B

Mousis, Olivier; Bouquet, Alexis; Waite, J. Hunter +1 more

The internal ocean of Enceladus can be expected to present conditions favorable to the trapping of volatiles in clathrates. This process could influence the eventual composition of the ocean and therefore of the plumes emitted by the south polar region. Here we used a statistical thermodynamic model to assess which species detected in the plumes b…

2015 Geophysical Research Letters
Cassini 51