Search Publications

Sodium chloride as a geophysical probe of a subsurface ocean on Enceladus
DOI: 10.1029/2010GL042446 Bibcode: 2010GeoRL..37.9204G

Glein, Christopher R.; Shock, Everett L.

Recent data from the Cassini spacecraft suggest that an ocean exists inside Saturn's satellite Enceladus. Here, we show that the size of an ocean can be estimated if the NaCl concentration of the ocean is known. We find that concentrations of aqueous NaCl reported by Postberg et al. (2009) imply a relatively large ocean, comprising at least 17% by…

2010 Geophysical Research Letters
Cassini 23
A strong high altitude narrow jet detected at Saturn's equator
DOI: 10.1029/2010GL045434 Bibcode: 2010GeoRL..3722204G

Hueso, R.; Sánchez-Lavega, A.; García-Melendo, E. +2 more

Here we report the discovery at the upper cloud level of an extremely narrow and strong prograde jet, centered in the middle of the broad equatorial jet. Measurements from images obtained by the Cassini Imaging Science Subsystem (ISS) show that the jet reaches 430 ms-1 ± 16 m s-1 with a peak speed difference of 180 ms-1<…

2010 Geophysical Research Letters
Cassini 22
Differences in solar wind cross-helicity and residual energy during the last two solar minima
DOI: 10.1029/2010GL044570 Bibcode: 2010GeoRL..3717102P

Perri, S.; Balogh, A.

The minimum of solar cycle 23 exhibited anomalous characteristics with respect to its predecessors. Other than the differences in the standard indicators of activity, such as sunspots, polar magnetic fields were also found to be different. These differences had a range of effects in the solar wind. In this work we study the Alfvénicity and the res…

2010 Geophysical Research Letters
Ulysses 22
Venus OH nightglow distribution based on VIRTIS limb observations from Venus Express
DOI: 10.1029/2010GL042377 Bibcode: 2010GeoRL..37.6805S

Drossart, P.; Piccioni, G.; Gérard, J. -C. +1 more

The full set of VIRTIS-M limb observations of the OH Venus nightglow has been analyzed to determine its characteristics. Based on 3328 limb profiles, we find that the mean peak intensity along the line of sight of the OH(Δv = 1 sequence) is 0.35-0.21+0.53 MR and is located at 96.4 ± 5 km. The emission is highly variable and n…

2010 Geophysical Research Letters
VenusExpress 20
Cassini imaging search rules out rings around Rhea
DOI: 10.1029/2010GL043663 Bibcode: 2010GeoRL..3714205T

Hedman, Matthew M.; Burns, Joseph A.; Tiscareno, Matthew S. +1 more

We have conducted an intensive search using the Cassini ISS narrow-angle camera to identify any material that may orbit Rhea. Our results contradict an earlier and surprising inference that Rhea, the second-largest moon of Saturn, possesses a system of narrow rings embedded in a broad circum-satellite disk or cloud.

2010 Geophysical Research Letters
Cassini 18
Escape of O+ through the distant tail plasma sheet
DOI: 10.1029/2010GL045075 Bibcode: 2010GeoRL..3721101K

Sauvaud, J. -A.; Wurz, P.; Bochsler, P. +13 more

In February 2007, the STEREO-B spacecraft encountered the magnetosheath, plasma sheet and plasma sheet boundary layer from about 200 RE to 300 RE downtail. This time period was during solar minimum, and there was no storm activity during this month. Using data from the PLASTIC instrument, we find that even during quiet times,…

2010 Geophysical Research Letters
Cluster 18
Groundwater processes in Hebes Chasma, Mars
DOI: 10.1029/2010GL044122 Bibcode: 2010GeoRL..3713202G

Grindrod, Peter M.; Balme, Matthew R.

We describe a conceptual model of groundwater processes at Hebes Chasma, Mars, which can account for the distribution of hydrated minerals and their subsequent evolution. At Hebes Chasma, pressure gradients set up by the large central mound, Hebes Mensa, could cause groundwater to be sourced predominantly from beneath the central region, if such w…

2010 Geophysical Research Letters
MEx 18
Permittivity estimation of layers beneath the northern polar layered deposits, Mars
DOI: 10.1029/2010GL043015 Bibcode: 2010GeoRL..3714201L

Orosei, Roberto; Cartacci, Marco; Cicchetti, Andrea +6 more

Martian Polar Layered Deposits, most likely dusty ice are transparent to radar waves. In the North Pole bedrock has been detected by MARSIS up to a depth about 2 Km, whereas in the South Pole such interface has been located at about 3.7 Km. The reflected signal is generally above the noise and can be used to estimate the dielectric properties of t…

2010 Geophysical Research Letters
MEx 17
Time-varying magnetospheric environment near Enceladus as seen by the Cassini magnetometer
DOI: 10.1029/2010GL042948 Bibcode: 2010GeoRL..37.9203J

Russell, C. T.; Dougherty, M. K.; Khurana, K. K. +3 more

In 2008, the Cassini spacecraft made four close Enceladus flybys along similar trajectories. During these flybys the magnetometer recorded the time-varying magnetic field associated with the plasma interaction with Enceladus and its plume. Close to Enceladus, the Cassini magnetometer observed 4% to 7% enhancement in the magnetic field magnitude, a…

2010 Geophysical Research Letters
Cassini 16
The spectrum of a Saturn ring spoke from Cassini/VIMS
DOI: 10.1029/2009GL041427 Bibcode: 2010GeoRL..37.1203D

Brown, R. H.; Nicholson, P. D.; Bellucci, G. +7 more

On 2008, July, the Cassini/VIMS spectrometer detected spokes on the Saturn's B ring for the first time. These are the first measurements of the complete reflectance spectrum of the spokes in a wide spectral range (0.35-0.51 µm). Here we will focus on a single broad-shaped spoke, imaged by VIMS on July, 9. Radiative transfer modeling supports…

2010 Geophysical Research Letters
Cassini 16