Search Publications

A dynamo model for axisymmetrizing Saturn's magnetic field
DOI: 10.1029/2009GL041752 Bibcode: 2010GeoRL..37.5201S

Stanley, S.

Magnetic field measurements demonstrate that Saturn's internally generated magnetic field has an extremely small dipole tilt. The nearly-perfect axisymmetry of Saturn's dipole is troubling because of Cowling's theorem which states that an axisymmetric magnetic field cannot be maintained by a dynamo. A possible mechanism to axisymmetrize the observ…

2010 Geophysical Research Letters
Cassini 33
Non-detection of impulsive radio signals from lightning in Martian dust storms using the radar receiver on the Mars Express spacecraft
DOI: 10.1029/2010GL044368 Bibcode: 2010GeoRL..3717802G

Gurnett, D. A.; Morgan, D. D.; Farrell, W. M. +3 more

Here we report the results of a nearly five-year search for impulsive radio signals from lightning discharges in Martian dust storms using the radar receiver on the Mars Express spacecraft. The search covered altitudes from 275 km to 1400 km and frequencies from 4.0 to 5.5 MHz with a time resolution of 91.4 µs and a detection threshold of 2.…

2010 Geophysical Research Letters
MEx 32
Saturn's periodic magnetic field perturbations caused by a rotating partial ring current
DOI: 10.1029/2010GL045285 Bibcode: 2010GeoRL..3722103B

Khurana, K. K.; Krimigis, S. M.; Mitchell, D. G. +7 more

We demonstrate that the periodic magnetic field perturbations as observed from Cassini are caused by the plasma pressure of the energetic (>2 keV) particle distributions that are periodically injected and subsequently drift around Saturn. Plasma pressures inferred from the Cassini Plasma Spectrometer (CAPS) (<2 keV) and the Magnetospheric Im…

2010 Geophysical Research Letters
Cassini 30
Influence of hot plasma pressure on the global structure of Saturn’s magnetodisk
DOI: 10.1029/2010GL045159 Bibcode: 2010GeoRL..3720201A

Coates, A. J.; Thomsen, M. F.; Wilson, R. J. +4 more

Using a model of force balance in Saturn's disk-like magnetosphere, we show that variations in hot plasma pressure can change the magnetic field configuration. This effect changes (i) the location of the magnetopause, even at fixed solar wind dynamic pressure, and (ii) the magnetic mapping between ionosphere and disk. The model uses equatorial obs…

2010 Geophysical Research Letters
Cassini 29
Electron beams as the source of whistler-mode auroral hiss at Saturn
DOI: 10.1029/2010GL042980 Bibcode: 2010GeoRL..37.9102K

Schippers, P.; André, N.; Gurnett, D. A. +8 more

Over the last three years, the Cassini spacecraft has been in a series of high inclination orbits, allowing investigation and measurements of Saturnian auroral phenomena. During this time, the Radio and Plasma Wave Science (RPWS) Investigation on Cassini detected low frequency whistler mode emissions propagating upward along the auroral field line…

2010 Geophysical Research Letters
Cassini 28
Correlations between cloud thickness and sub-cloud water abundance on Venus
DOI: 10.1029/2009GL041770 Bibcode: 2010GeoRL..37.2202T

Drossart, Pierre; Irwin, Patrick G. J.; Piccioni, Giuseppe +6 more

Past spacecraft observations of Venus have found considerable spatial and temporal variations of water vapour abundance above the clouds. Previous searches for variability below the clouds at 30-45 km altitude found no large scale latitudinal gradients, but lacked the spatial resolution to detect smaller scale variations. Here we interpret results…

2010 Geophysical Research Letters
VenusExpress 27
SAID: A turbulent plasmaspheric boundary layer
DOI: 10.1029/2010GL042929 Bibcode: 2010GeoRL..37.7106M

Santolik, O.; Mishin, E. V.; Puhl-Quinn, P. A.

This paper presents novel features of subauroral ion drifts (SAID) observed from a unique conjunction of the Cluster, DMSP, and Polar satellites, including the discovery of SAID-related plasma waves. These observations confirm and expand on our proposed concept of the SAID channel being a turbulent boundary layer, formed via a short circuit of the…

2010 Geophysical Research Letters
Cluster 27
Modeling the Enceladus plume-plasma interaction
DOI: 10.1029/2009GL041613 Bibcode: 2010GeoRL..37.3202F

Delamere, P. A.; Bagenal, F.; Fleshman, B. L.

We investigate the chemical interaction between Saturn's corotating plasma and Enceladus' volcanic plumes. We evolve a parcel of ambient plasma as it passes through a prescribed H2O plume using a physical chemistry model adapted for water-group reactions. The flow field is assumed to be that of a plasma around an electrically-conducting…

2010 Geophysical Research Letters
Cassini 27
Climbing and falling dunes in Valles Marineris, Mars
DOI: 10.1029/2009GL042263 Bibcode: 2010GeoRL..37.8201C

Chojnacki, Matthew; Moersch, Jeffrey E.; Burr, Devon M.

Multiple occurrences of “wall dunes” are found several kilometers above the Valles Marineris canyon floor. Dune slip face orientation and bed form morphologies indicate transport direction and whether the wall dunes are climbing dunes or falling dunes. On Earth, these types of dunes form in a unidirectional wind regime and are strongly controlled …

2010 Geophysical Research Letters
MEx 26
Impact-induced overland fluid flow and channelized erosion at Lyot Crater, Mars
DOI: 10.1029/2010GL045074 Bibcode: 2010GeoRL..3721201H

Harrison, Tanya N.; Malin, Michael C.; Cantor, Bruce A. +5 more

Lyot Crater is one of the youngest impact basins > 200 km in diameter on Mars. Although published hydrological models suggest that impact-related groundwater release might have occurred at Lyot, no geomorphic evidence for such activity has been previously identified. Here, we use images acquired predominantly by the Mars Reconnaissance Orbiter …

2010 Geophysical Research Letters
MEx 23